This repository contains a seismic event catalog that has 60,006 events within the Antarctic continent between January 1, 2000 to January 1, 2021, with event moment magnitudes between -1 to 4.5. The catalog is in csv format. The catalog contains events from different sources including icequakes, volcanic events, and tectonic earthquakes.
\nCurrently, a manuscript has been submitted to Seismological Research Letters: Data Mine, where we explained the methods used to obtain the catalog. The manuscript has not been peer reviewed yet. We will updated the catalog and repository if there are any changes.
\nThe repository also contains an excel file that list all the seismic networks we use in our study.
","url":"https://doi.org/10.5281/zenodo.10710522","contact":"Pena Castro, Andres Felipe, Schmandt, Brandon, Nakai, Jenny, Aster, Rick, Chaput, Julien","deadline":"2024-02-26","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":1440,"type":"dataset","title":"Altimeter-Derived Geostrophic Velocities Across the Northeast Channel; Indices for Scotian Shelf Crossovers","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,dataset,Gulf of Maine,Scotian Shelf Crossovers,Geostrophic Velocities,Northeast Channel","description":"Dataset.This dataset consists of two indices quantifying the geostrophic cross-channel velocity across the Northeast Channel in the Gulf of Maine derived from altimeter data. The purpose of these indices is to quantify the occurrences of Scotian Shelf Crossover events in which water cuts directly across the Northeast Channel from the Scotian Shelf to Georges Bank instead of traveling around the Gulf of Maine.
\nThe first index was generated DUACS delayed-time altimeter gridded maps with a spatial resolution of 1/4 degree available from Copernicus Marine Services (https://doi.org/10.48670/moi-00145). We used the absolute geostrophic velocity supplied from the DAUCS product, which is calculated from the absolute dynamic topography. We isolated a region spanning across the NEC, which includes 48 of the SSH grid points (shown as the red box in the included figure). For each grid point within this box, the cross-channel component of the velocity was calculated, with the 500m isobath being the cross-channel direction. The angle () between the 500m isobath and the geostrophic velocity from the gridded SSH product was calculated and used to find the cross-shelf component of the velocity, with the following equation where is the total geostrophic velocity and","url":"https://doi.org/10.5281/zenodo.20940948","contact":"Silver, Adrienne, Gawarkiewicz, Glen, Oliver, Hilde","deadline":"2026-06-26","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":1421,"type":"dataset","title":"Catalog of icequakes recorded in March 2019, in the Van Mijen Fjord, in Svalbard (Norway)","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,dataset","description":"Dataset. The files contain a catalog of icequakes waveforms recorded in March 2019, at Vallunden lake, in the Van Mijen Fjord, in Svalbard (Norway). The three components of velocity are available. Authors: Tifenn Le Bris1, Guilhem Barruol1, Florent Gimbert1, Emmanuel Le Meur1, Dimitri Zigone2,3, Maxime Bès de Berc2, Armelle Bernard3 Univ. Grenoble Alpes, CNRS, INRAE, IRD, Grenoble INP, IGE, 38000 Grenoble, France Université de Strasbourg/CNRS, Institut Terre et Environnement de Strasbourg, UMR7063, 67084 Strasbourg Cedex, France Université de Strasbourg/CNRS, Ecole et Observatoire des Sciences de la Terre, UAR830, 67084 Strasbourg Cedex, France Corresponding author: Tifenn Le Bris (tifenn.le-bris@univ-grenoble-alpes.fr) This dataset belongs to the study of Nanni et al., 2020 "Quantification of seasonal and diurnal dynamics of subglacial channels using seismic observations on an Alpine Glacier." accepted for publication in The Cryosphere on March 9th 2020. You can find additional information on the "README_data_NANNI_2020_glacier" This dataset contains DEMs, elevation change data, subsets of downscaled CMIP6 data (Coupled Model Intercomparison Project, Phase 6), snowfall measurements collected by Whistler Blackcomb, and BC weather station data used to calculate lapse rates and build a positive degree-day (PDD) model for Whistler, Horstman and Blackcomb glaciers, located in British Columbia, Canada. Outlines of these glaciers between 1973 and 2024 are also provided for these glaciers. For more details see: Monty C, Flowers GE, Crompton JW, Menounos B, Mathias C. On the demise of Whistler, Horstman and Blackcomb Glaciers, southwest British Columbia, Canada: historical use, recent change and future prospects within a mountain resort. Annals of Glaciology. 2026;67:e19. doi:10.1017/aog.2026.10045 This dataset compiles 243,753 daily groundwater chloride concentration observations from 46,289 monitoring wells across 13 U.S. Atlantic and Gulf Coast states (AL, DE, FL, GA, LA, MD, MS, NC, NJ, PA, SC, TX, VA), spanning 1906 to 2023. Each observation is enriched with a comprehensive set of static hydrogeological, dynamic tidal, and climatic predictors assembled from federal and state sources. The dataset was developed to support the research paper Predicting salinization of groundwater along the U.S. Atlantic and Gulf coasts with machine learning, as described in Tian et al. (2026, Water Resources Research). All observations were located within approximately 160 km (100 miles) of the coastline, as defined by the uploaded study area file. This dataset provides daily discharge time series collected from multiple rock glacier springs and upstream mountain rivers across the Austrian Alps. Characterizing the hydrologic regimes of headwaters is critical for understanding water availability and storage dynamics in alpine environments. This high-elevation field dataset complements nearby lower-altitude downstream river gauging stations operated by the Hydrographic Service of Austria, TIWAG, and illwerke vkw, providing the critical upstream component necessary for whole-catchment water balance assessments. Data Structure and Format: The dataset is organized into individual CSV files. Each file is named using the convention [MountainRange]_[Location].csv. The internal structure of each file is contains date and discharge (reported in liters per second). This open-access dataset serves as a baseline for alpine hydrologic modeling, cryospheric water resource assessments, and hydrogeochemical studies in the European Alps. Dalk_clustering_events.tar.gz contains 909,720 events' waveforms detected near Dalk Glacier, in the Larsemann Hills, East Antarctica from 6 Dec 2019 to 2 Jan 2020. Original seismic data are recorded by 100 three-component short-duration seismometers. The preprocessing includes detrending, tapering and 1-Hz high-pass filtering and the detection method is STA/LTA (short term=0.5 s, long term=30 s, trigger threshold=10, detrigger threshold=3). unsupervised_clustering_code.zip contains the python codes of detecting by STA/LTA, feature extraction by an autoencoder and clustering by a Gaussian mixture model. Data associated with the submitted manuscript titled: Icequake rupture suggests Antarctic ice stream beds may be stronger, yet more dynamic than previously assumed (authors: T.S. Hudson, A.M. Brisbourne and L.K. Zoet). Contains: iq_rupture_results_FINAL_FOR_PUBLICATION.csv - A file containing rupture velocity inversion results and auxilary information for all icequakes used in the analysis. header_descriptions.txt - A file containing decriptions of every parameter contained in iq_rupture_results_FINAL_FOR_PUBLICATION.csv. Data associated with the study: Unlocking DAS amplitude information through coherency coupling quantification Here we include all DAS data used in the study that is not included in an open access repository elsewhere. Contents of this repository are: Gornergletscher data: High pathogenicity avian influenza (HPAI) viruses have rapidly emerged as a major global threat to wildlife, with severe consequences for seabird populations. Albatrosses and petrels (order Procellariiformes) are particularly vulnerable due to their long lifespan, low reproductive rates and strong site fidelity. Since 2021, HPAI viruses have caused unprecedented mortality in seabird communities worldwide and have expanded into the core range of procellariiform species, including sub-Antarctic and Antarctic regions. In response to the urgent need for timely, species-relevant information, the Agreement on the Conservation of Albatrosses and Petrels (ACAP) established the High Pathogenicity H5Nx Avian Influenza Intersessional Correspondence Group (HPAI-ICG), which developed the ACAP HPAI database — an openly accessible, regularly updated resource that consolidates all known suspected and confirmed HPAI events involving procellariiform birds. The database compiles information from global and national reporting systems, scientific literature, genetic repositories, government communications and direct expert notifications. Events are standardised using transparent case definitions, cross-referenced and validated by subject-matter experts and complemented by additional data on case impacts and viral characteristics. The database provides a critical decision-support tool for governments, rese","url":"https://doi.org/10.5281/zenodo.20944655","contact":"Vanstreels, Ralph E. T., Serafini, Patricia P., Giacinti, Jolene, Younger, Jane, Huyvaert, Kathryn P., Wille, Michelle, Roberts, Laura, Gamble, Amandine","deadline":"2026-06-26","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":1407,"type":"dataset","title":"Dataset Publication for \"A repeating earthquake catalog for the Atacama Sement in North Chile (24.5°S-30.5°S)\"","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,dataset,Repeating Earthquakes,Catalog,subduction zone,creeping faults","description":"Dataset. This is the repeating earthquake catalog data described in \"A repeating earthquake catalog for the Atacama Segment Northern Chile\", submitted to Seismica. In the following, the three contained files are described: nca_repeater_list.txt Repeater list for North Chile Atacama, 1998-2024 time : event origin time nca_mining_cluster_list.txt List of mining clusters identified via TM for Nort","url":"https://doi.org/10.5281/zenodo.20825955","contact":"Folesky, Jonas","deadline":"2026-06-24","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":1413,"type":"dataset","title":"Dataset associated with the manuscript: Quantifying subsurface fracture damage in glaciers using fibre-optic seismology","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,dataset","description":"Dataset. This data repository contains the core data and scripts required to preproduce the work presented in the publication titled \"Quantifying subsurface fracture damage in glaciers using fibre-optic seismology\" by Thomas Hudson, Fabian Walter, Sebastian Noe, Andrea Zunino, John-Michael Kendall, Pascal Edme, and Andreas Fichtner. Note that due to data volume constraints, we do not include the raw seismic data here. The entire dataset is of the order of 2 TB, but we will endevour to make it available upon request. The repository contains the following files: The following data is included here, which comprises the data presented in the publication: Files included are: Headers for the files are as follows: The dataset \"raw_DAS\" contains cryoseismological distributed acoustic sensing (DAS) data recorded in July 2020 on Rhône Glacier, Switzerland. The dataset \"training_data\" contains raw and preprocessed seismometer recordings used as training data, also recorded in July 2020 on Rhône Glacier, Switzerland. These datasets provide the necessary data to reproduce the results presented in the paper “Self-Supervised Coherence-Based Denoising of Cryoseismological Distributed Acoustic Sensing Data.” The corresponding code is available on GitHub, and the paper can be accessed via Authorea. Abstract A major challenge in cryoseismology is that signals of interest are often buried within the high noise level emitted by a variety of environmental processes. Particular Distributed Acoustic Sensing (DAS) data often suffers from low signal-to-noise ratios (SNR) potentially resulting in a multitude of undetected events of interest, which further remain unanalyzed. To record seismicity, we deployed a DAS system on Rhône Glacier, Switzerland, using a 9 km long fiber-optic cable that covered the entire glacier, from its accumulation to its ablation zone. The highly active and dynamic cryospheric environment, in combination with poor coupling, resulted in DAS data characterized by a low SNR. Our objective is to develop and evaluate a method to effectively de","url":"https://doi.org/10.5281/zenodo.14998653","contact":"Zitt, Johanna","deadline":"2025-03-10","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":1395,"type":"dataset","title":"Dataset for the manuscript \"Self-Supervised Coherence-Based Denoising on Cryoseismological Distributed Acoustic Sensing Data\"","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,dataset,cryoseismology,distributed acoustic sensing,denoising,Rhonegletscher","description":"Dataset. The dataset contains cryoseismological data recorded in July 2020 on the Rhonegletscher, Switzerland, collected using both Distributed Acoustic Sensing and seismometers. Abstract: One major challenge in cryoseismology is that signals of interest are often buried within the high noise level emitted by a multitude of environmental processes. Events of interest potentially stay unnoticed and remain unanalyzed, particularly because conventional sensors cannot monitor an entire glacier. However, with Distributed Acoustic Sensing (DAS), we can observe seismicity over multiple kilometers. DAS systems turn common fiber-optic cables into seismic arrays that measure strain rate data, enabling researchers to acquire seismic data in hard-to-access areas with high spatial and temporal resolution. We deployed a DAS system on Rhonegletscher, Switzerland, using a 9 km long fiberoptic cable that covered the entire glacier, from its accumulation to its ablation zone, recording seismicity for one month. The highly active and dynamic cryospheric environ ment, in combination with poor coupling, resulted in DAS data characterize","url":"https://doi.org/10.5281/zenodo.13868934","contact":"Zitt, Johanna","deadline":"2024-10-01","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":1392,"type":"dataset","title":"Denoised data for the manuscript \"Self-Supervised Coherence-Based Denoising of Cryoseismological Distributed Acoustic Sensing Data\"","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,dataset,cryoseismology,distributed acoustic sensing,denoising,Rôhne Glacier,J-invariance","description":"Dataset. These datasets provide the necessary data to reproduce the results presented in the paper “Self-Supervised Coherence-Based Denoising of Cryoseismological Distributed Acoustic Sensing Data.” The corresponding code is available on GitHub, and the paper can be accessed via Authorea. The data set \"02_accumulation_denoisedDAS\" contains the denoised data of the model J-invariant-cryo-acc. Abstract: A major challenge in cryoseismology is that signals of interest are often buried within the high noise level emitted by a variety of environmental processes. Particular Distributed Acoustic Sensing (DAS) data often suffers from low signal-to-noise ratios (SNR) potentially resulting in a multitude of undetected events of interest, which further remain unanalyzed. To record seismicity, we deployed a DAS system on Rhône Glacier, Switzerland, using a 9 km long fiber-optic cable that covered the entire glacier, from its accumulation to its ablation zone. The highly active and dynami","url":"https://doi.org/10.5281/zenodo.14999918","contact":"Zitt, Johanna","deadline":"2025-03-10","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":1394,"type":"dataset","title":"Denoised data for the manuscript \"Self-Supervised Coherence-Based Denoising on Cryoseismological Distributed Acoustic Sensing Data\"","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,dataset","description":"Dataset. This dataset contains denoised sections of Distributed Acoustic Sensing (DAS) data, generated using a J-invariant autoencoder. It facillitates the reproduction of the results presented in the paper \"Self-Supervised Coherence-Based Denoising on Cryoseismological Distributed Acoustic Sensing Data.\" This is an export of the Sites and Monuments Record (Fornminnesinformationssystemet, FMIS), by the Swedish National Heritage Board, NHB (Riksantikvarieämbetet, RAÄ) that has later been replaced by the new Historic Environment Record, HER (Kulturmiljöregistrert, KMR). With the transition from FMIS to KMR, changes in the data structure and information content were carried out be NHB/RAÄ - https://www.raa.se/hitta-information/fornreg/handledningar-och-manualer-for-fornreg/forandringar-av-lamningsinformationen/ This dataset is thus published as a way to represent some of the information previously available. The current version of HER/KMR is available from: https://www.raa.se/hitta-information/oppna-data/oppna-data-portal/ This dataset lists the groundwater monitoring data for the Besos Delta Aquifer and River during the years 2023-2025, taken during the UPWATER project. The parameters measured were: Electrical conductivity, temperature, pH, oxygen, alkalinity, dissolved organic carbon, cloride, bicarbonate, sulfate, calcium, magnesium, nitrate, ammonia, potassium, sodium, phosphate, sulfur, boron,barium, strontium, vanadium, chromium, iron, manganese, cobalt, nickel, copper, aluminum, arsenic, zink, cadmium, lead, as well as isotopes of nitrate, water, sulfate, boron and carbonate. White-sky glacier albedo for Heard Island (53°06′S, 73°31′E), derived from NASA VIIRS VNP43 BRDF/albedo parameters for January 2012 to May 2024. Provides a glacier-wide area-mean albedo time series (4,466 valid daily broadband white-sky albedo records; mean 0.343 ± 0.062; range 0.037–0.723) and annual albedo rasters (2012–2024, GeoTIFF), with the ERA5-Land daily climate and SRTM elevation inputs and the GLIMS glacier outline used in the analysis. Temporal availability ≈ 98.9 % of study-period days; spatial coverage 44.04 % of glacier area (cloud-limited). Analysis code (Google Earth Engine + R) and per-file column definitions (DATA_DICTIONARY.md) are included. Data licensed CC BY 4.0; code under MIT. This deposit is the data and code archive for the Scientific Data Data Descriptor \"Heard Island glacier albedo from VIIRS satellite observations 2012 to 2024\" (under review). Icequakes detected using array-based method and network-based method, associated with the publication: Hudson, T. S., Brisbourne, A. M., Kufner, S., Kendall, J., & Smith, M. (2023). Array processing in cryoseismology. Submitted to: The Cryosphere. For the network earthquake catalogue, t0 refers to the origin time of an icequake. For the array earthquake catalogue, t_P and t_S refer to the P and S wave arrival times of an icequake. Also included is a csv file containing the seismic velocity model used in the analysis. This is a subset of open access data from the following reference; please cite accordingly: Walter, F. (2009). Seismic activity on gornergletscher during gornersee outburst floods. Dissertation, 31(1-2), 14–27. https://doi.org/10 .1007/BF03322148 Curated by T. Sawi for the manuscript (in submission): An Unsupervised Machine-Learning Approach to Understanding Seismicity at an Alpine Glacier; by T. Sawi; B. Holtzman; M. Nettles; F. Walter; J. Paisley; submitted to JGR: Earth Surface in August 2022. This data set contains two-second records of shallow (<50 m depth) glacial icequakes (N=1,460) from the vertical channel of a Geospace GS-11D geophone operating in shallow borehole at Gornergletscher between June 14 and July 22, 2007. Sampling rate is 1000 samples per second, and the natural frequency of the instrument is around 8 Hz. An STA/LTA filter has been applied to attempt to remove records with more than one prominent icequake in them. Waveform files are named after their event origin time in format 7{MDhms}. For example, waveform "70614004000.gse2" occurred on June 14 00:40:00, 2007. This dataset contains the input pickle file used for river discharge modeling with LSTM and LSTM + mTAN models under gauged and ungauged settings. The pickle file is an OrderedDict with COMID values as the top-level keys. Each COMID contains a NumPy array of dates and a data tensor containing discharge, predictor variables, and water surface elevation (WSE). A separate README_input_pickle_file.txt file describes the column order and contents of the pickle file. Time-lapse camera images of the Perito Moreno Glacier front used in this study, along with the seismic catalog of calving events obtained through template-matching analysis. This dataset supports the consensus moment tensor (MT) method developed at the European-Mediterranean Seismological Centre (EMSC) and described in Bossu et al. (2026). For many earthquakes, several MT solutions are reported by different seismological agencies using different networks and inversion methods. The consensus approach of Bossu et al. (2026) computes a provider-neutral, reproducible representative solution per earthquake by applying robust median/MAD statistics to solutions compared with two complementary metrics: the Kagan (1991) rotation angle (double-couple geometry) and the Rivera–Kanamori (RK) similarity (Rivera & Kanamori, 2014). The repository contains six files: a README, one raw input file, two global consensus result files, and two files specific to the Tonga region case study. **File 1:** `mt_seismicportal_20140101-20260430.json` (53Mo) — Raw input dataset retrieved from the EMSC SeismicPortal. Covers 10,650 seismic events with 34,425 moment tensor solutions (minimum 2 solutions per event), contributed by 28 agencies worldwide, for the period 2014-01-01 to 2026-04-30. Each event includes hypocenter parameters and, for each contributing agency, centroid location, scalar moment, moment magnitude, nodal planes, full tensor components, principal axes, and source decomposition (Vavryčuk, 2015). **File 2:** `consensus_kagan_run_prefilt-31_strictMAD-publish-17-final.json` (40Mo) — Consensus results us","url":"https://doi.org/10.5281/zenodo.20528206","contact":"European-Mediterranean Seismological Centre, Bossu, Rémy, Roch, Julien, Landès, Matthieu, Ucciani, Guillaume","deadline":"2026-06-11","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:44:55.032906","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1437,"type":"dataset","title":"Product Desirability Toolkit Listing: Results from a Systematic Mapping Study","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,dataset,Human Computer Interaction (HCI),User Experience,Desirability,Product Desirability Toolkit,Systematic Mapping Study","description":"Dataset. This listing contains a total of 551 scholarly articles, published between 2002 and June 2026 that used the Product Desirability Toolkit (PDT) in some way. In the future, we plan to categorize the listing and provide a brief outline for each article along with a link. This listing serves as both a comprehensive repository of existing PDT work, and as a starting point for adding new PDT- related research to the list. Contact the first author to add a CSO GA to the next version of the list. The listing was gathered using a methodical, comprehensive literature review using the Systematic Mapping Study (SMS) process to identify implemented and evaluated scholarly articles that used the PDT (in submission). Using traditional SMS approaches, our study was conducted May-June 2026 and searched for English literature published between 2002 and mid 2026, which made the use of the PDT, and found 550 scholarly works in total. Google Scholar noted 525 citations from the original Bendek and Miner 2002 source, but after pruning for missing author, year, title data, 458 works resulted. Scopus found 342 total scholarly papers/books from the citation after pruning, with 41 unique works there were not in the Google Scholar listing, and an additional 12 works that did not directly cite the original paper. ACM digital library and IEEE added 3 and 4 unique works, respectively. Using the PublishOrPerish to","url":"https://doi.org/10.5281/zenodo.20964948","contact":"Weitl-Harms, Sherri, Hastings, John","deadline":"2026-06-27","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":1411,"type":"dataset","title":"Resources for the REASSESS paper on Low Frequency Icequakes during cavity drainages","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,dataset","description":"Dataset. This dataset contains data and codes used for the paper \"Low frequency icequakes generated during transient cavity drainage on a Greenlandic outlet glacier\". Following files are provided: All this data can be used with the provided Python code, which corresponds to the code used to generate the respective figures in the paper: Figure1.py, Figure2a.py, Supplementary repository for manuscript: This repository contains data and metadata for interested parties to reproduce seismic event analyses for 21915 events classified as basal icequakes recorded between August 1st and 19th 2019 at Saskatchewan Glacier, Alberta, Canada. This is a subset of open access data from the following reference; please cite accordingly: Walter, F. (2009). Seismic activity on gornergletscher during gornersee outburst floods. Dissertation, 31(1-2), 14–27. https://doi.org/10 .1007/BF03322148 Curated by T. Sawi for the manuscript (in submission), "An Unsupervised Machine-Learning Approach to Understanding Seismicity at an Alpine Glacier" (2022) by T. Sawi; B. Holtzman; M. Nettles; F. Walter; J. Paisley; submitted to JGR: Earth Surface in August 2022. This data set contains sixty-second samples of glacial seismic noise (N=1,478) from the vertical channel of a Geospace GS-11D geophone operating in shallow borehole at Gornergletscher between June 14 and July 22, 2007. Sampling rate is 1000 samples per second, and the natural frequency of the instrument is around 8 Hz. An STA/LTA filter has been applied to remove records with prominent icequakes in them, although many smaller icequakes remain in the records. Waveform files are named after their event origin time in format 7{MDhms}. For example, waveform "70614004000.sac" occurred on June 14 00:40:00, 2007. This deposit contains the data set we used in our paper ‘Dynamic imaging of glacier structures at high-resolution using source localization with a dense seismic array’. The paper is in review for GRL and a preprint can be found here: 10.1002/essoar.10507953.1. The dataset present here contains 34 files named ‘beam_15423_jd***.h5’. These files correspond to the output of the matched field processing for each day. They are in .h5 format and we provide a matlab code (read_MFP_data.m) to read these files. These files can be read with any other language since they are in . h5. In linux you can use h5dump –A filename.h5 and you can see the content of each files. More information on how the MFP process is conducted can be found in on the website dedicated to this aspect or on our paper. The whole procedure and associated codes is provided on the lecoinal.gricad-pages.univ-grenoble-alpes.fr/resolve/. We also deliver with this deposit one day of seismic data ZO_2018_121.h5 A single-band, 16-bit ice-adapted normalised-difference water-index image of supraglacial melt ponds on the south-west Greenland ice sheet, prepared as the Earth-observation input for the Galaxy Training Network tutorial Introduction to Image Analysis using Galaxy (gxy.io/GTN:T00181). NDWIice = (blue − red)/(blue + red) (Williamson et al. 2018, doi:10.5194/tc-12-3045-2018), computed from a Sentinel-2 Level-2A scene (tile T22WEV, 2019-07-23) over the Russell–Leverett ablation zone and rescaled to 16-bit so that melt ponds are the bright objects — the Earth-observation analogue of the bright cell nuclei the tutorial uses. The same threshold → label → count steps then count melt ponds. Full provenance, the preprocessing pipeline, the Galaxy run, and validation against an independently published lake map are in the OSCARS–FIESTA example repository: annefou/fiesta-galaxy-meltponds-eo. Contains modified Copernicus Sentinel data 2019. These archives contain annual mass balance and related variables for Glacier AX010 in the SHorong region, Nepal Himalaya, for the period from 1941 to 2023. Annual variables are outputs for the period from 1 Oct. to 30 Sep. Control result (mb_ctl.csv) denotes the mass balance simulated with the precipitation parameter (r_P=1.48) tuned to yield the observed geodetic mass balance. Also shown are the results with the lower (_ngt) and upper (_pst) bounds of the parameter (+/- 0.08). Results simulated without calibrating precipitation parameter are also provided (_nc). Files Description of the datasheet Citation: Fujita K, Kayashta RB (in review) Temperature-driven shrinkage of a disappearing Himalayan glacier. The Cryoshpere. Output from four global JULES simulations as described in Future global water scarcity partially moderated by vegetation responses to rising CO₂ (Stacey et al., 2025; DOI: 10.5194/egusphere-2025-51). The simulations have been used to explore the effects of vegetation and plant physiological responses to rising atmospheric CO₂ by combining experiments in which the dynamic vegetation scheme (TRIFFID) and stomatal conductance (plant–CO₂ response) are either enabled or fixed. The dataset contains monthly output for multiple hydrological and vegetation-related variables for the historical period 1900–2005 and the future period 2006–2100 under the RCP6.0 scenario. Simulations were performed using the JULES-ES ISIMIP2b configuration. Details of the model setup are provided in Description and evaluation of the JULES-ES set-up for ISIMIP2b (Mathison et al., 2023). All simulations were conducted without land-use change. Data are supplied in NetCDF format. The dataset supports the analyses presented in Stacey et al. (2025; DOI: 10.5194/egusphere-2025-51). Code used to process, analyse, and visualise the data is available from the associated GitHub repository. Funding: Met Office Hadley Centre Climate Programme, funded by the UK Department for Science, Innovation ","url":"https://doi.org/10.5281/zenodo.20826090","contact":"Stacey, Jessica","deadline":"2026-06-24","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":183,"type":"dataset","title":"NASA Earthdata Cryosphere","institution":"NASA","country":"United States","city":"","latitude":null,"longitude":null,"tags":"dataset,nasa,cryosphere,remote sensing,ice","description":"NASA Earthdata access point for cryosphere-related datasets.","url":"https://www.earthdata.nasa.gov/topics/cryosphere","contact":"","deadline":"","source":"official","priority":9,"created_at":"2026-06-27T21:14:20.694103","quality_score":88,"quality_reason":"priority=9, has_url, official_like_url, trusted_source, good_tags"},{"id":32,"type":"dataset","title":"NSIDC Data Search","institution":"NSIDC","country":"United 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Verify details, deadline and eligibility on the official page.","url":"https://www.bas.ac.uk/data/polar-data-centre/data-deposit/","contact":"","deadline":"","source":"https://www.bas.ac.uk/jobs/vacancies/","priority":6,"created_at":"2026-06-27T21:10:56.549880","quality_score":83,"quality_reason":"priority=6, has_url, official_like_url, good_description, good_tags, high_value_type"},{"id":58,"type":"opportunity","title":"Field work","institution":"British Antarctic Survey Jobs","country":"United Kingdom","city":"","latitude":null,"longitude":null,"tags":"jobs,antarctica,bas,polar","description":"Potential opportunity found on British Antarctic Survey Jobs. 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Verify details, deadline and eligibility on the official page.","url":"https://fa-evzn-saasfaukgovprod1.fa.ocs.oraclecloud.com/hcmUI/CandidateExperience/en/sites/CX/job/2490","contact":"","deadline":"","source":"https://www.bas.ac.uk/jobs/vacancies/","priority":6,"created_at":"2026-06-27T21:10:56.549880","quality_score":68,"quality_reason":"priority=6, has_url, good_description, good_tags, high_value_type"},{"id":62,"type":"opportunity","title":"Going South","institution":"British Antarctic Survey Jobs","country":"United Kingdom","city":"","latitude":null,"longitude":null,"tags":"jobs,antarctica,bas,polar","description":"Potential opportunity found on British Antarctic Survey Jobs. 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Verify details, deadline and eligibility on the official page.","url":"https://www.bas.ac.uk/polar-capabilities/","contact":"","deadline":"","source":"https://www.bas.ac.uk/jobs/vacancies/","priority":6,"created_at":"2026-06-27T21:10:56.549880","quality_score":83,"quality_reason":"priority=6, has_url, official_like_url, good_description, good_tags, high_value_type"},{"id":1349,"type":"publication","title":"A fast and simplified subglacial hydrological model for the Antarctic Ice Sheet and outlet glaciers","institution":"HAL","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,","description":"Abstract. We present a novel and computationally efficient subglacial hydrological model that represents in a simplified way both hard- and soft-bed rheologies, as well as an automatic switch between efficient and inefficient subglacial discharge, designed for the Antarctic Ice Sheet. The subglacial model is dynamically linked to a regularized Coulomb friction law, allowing for a coupled evolution of the ice sheet on decadal to centennial timescales. It does not explicitly simulate the details of water conduits at the local scale and assumes that subglacial hydrology is in quasi-static equilibrium with the ice sheet, which makes the computations very fast. The hydrological model is tested on an idealized marine ice sheet and subsequently applied to the drainage basin of Thwaites Glacier, West Antarctica, that is composed of a heterogeneous (hard/soft) bed. We find that accounting for subglacial hydrology in the sliding law accelerates the grounding-line retreat of Thwaites Glacier under present-day climatic conditions. Highest retreat rates are obtained for hard-bed configurations and/or inefficient drainage systems. We show that the sensitivity is particularly driven by large gradients in effective pressure, more so than the value of effective pressure itself, in the vicinity of the grounding line. Therefore, we advocate for a better understanding of the subglacial system with respect to both the spatial and temporal variability in effective pressure and the rheological cond","url":"https://hal.science/hal-04966269v1","contact":"Elise Kazmierczak, Thomas Gregov, Violaine Coulon, Frank Pattyn","deadline":"2024","source":"HAL","priority":7,"created_at":"2026-06-27T21:51:45.375730","quality_score":0,"quality_reason":""},{"id":1339,"type":"publication","title":"A minimal machine-learning glacier mass balance model","institution":"Institut des Géosciences de l’Environnement","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,","description":"Glacier retreat presents significant environmental and social challenges. Understanding the local impacts of climatic drivers on glacier evolution is crucial, with mass balance being a central concept. This study introduces miniML-MB, a new minimal machine-learning model designed to estimate annual point surface mass balance (PMB) for very small datasets. Based on an eXtreme Gradient Boosting (XGBoost) architecture, miniML-MB is applied to model PMB at individual sites in the Swiss Alps, emphasising the need for an appropriate training framework and dimensionality reduction techniques. A substantial added value of miniML-MB is its data-driven identification of key climatic drivers of local mass balance. The best PMB prediction performance was achieved with two predictors: mean air temperature (May–August) and total precipitation (October–February). miniML-MB models PMB accurately from 1961 to 2021, with a mean absolute error (MAE) of 0.417 m w.e. across all sites. Notably, miniML-MB demonstrates similar and, in most cases, superior predictive capabilities compared to a simple positive degree-day (PDD) model (MAE of 0.541 m w.e.). Compared to the PDD model, miniML-MB is less effective at reproducing extreme mass balance values (e.g. 2022) that fall outside its training range. As such, miniML-MB shows promise as a gap-filling tool for sites with incomplete PMB measurements as long as the missing year's climate conditions are within the training range. This study underscores pot","url":"https://hal.inrae.fr/hal-05450616v1","contact":"Marijn van der Meer, Harry Zekollari, Matthias Huss, Jordi Bolibar, Kamilla Hauknes Sjursen, Daniel Farinotti","deadline":"2025","source":"HAL","priority":7,"created_at":"2026-06-27T21:51:45.375730","quality_score":0,"quality_reason":""},{"id":1334,"type":"publication","title":"Accurate Estimations of Sea-Ice Thickness and Elastic Properties From Seismic Noise Recorded With a Minimal Number of Geophones: From Thin Landfast Ice to Thick Pack Ice","institution":"Institut des Sciences de la Terre","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,seismic noise,monitoring,sea ice,seismic noise","description":"Despite their high potential for accurate sea ice properties estimation, seismic methods are still limited by the difficulty of access and the challenging logistics of polar environments. Conventional seismic methods generally require tens of geophones together with active seismic sources for monitoring applications. While this is not an issue for mainland environment, it is restrictive for sea ice and prevents long-term monitoring. We introduce a method to estimate sea ice thickness and elastic properties from passive recordings of the ambient seismic field with a minimal number of geophones. In comparison with our previous work (Moreau et al., 2020; https://doi.org/10.1029/2019JC015709) where about 50 sensors were used, the number of geophones is reduced by 1 order of magnitude, thanks to a new strategy of inversion of the passive seismic data. The method combines noise interferometry for estimating the elastic properties, with a Bayesian inversion of the dispersion in the waveforms of icequakes for inferring ice thickness, based on passive recordings from only 3-5 geophones, depending on the signal to noise ratio. We demonstrate its potential both on data recorded on thin landfast ice in Svalbard, and on data recorded on thick pack ice in the Arctic ocean.","url":"https://insu.hal.science/insu-03594474v2","contact":"Ludovic Moreau, Jérôme Weiss, David Marsan","deadline":"2020","source":"HAL","priority":7,"created_at":"2026-06-27T21:51:45.375730","quality_score":0,"quality_reason":""},{"id":1217,"type":"publication","title":"Age, thinning and spatial origin of the Beyond EPICA ice from a 2.5D ice flow model","institution":"Institut des Géosciences de l’Environnement, British Antarctic Survey","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,glaciology,ice cores,ice flow,chronology","description":"The Beyond EPICA Oldest Ice project is a European project that aims to retrieve a continuous ice core up to 1.5 Ma through deep drilling at Little Dome C (LDC), Antarctica. In order to determine the age of the ice at a given depth before the ice is analysed in detail, 1D numerical models are often employed. However, they do not take into account any effects due to horizontal ice flow. We present a 2.5D inverse model that determines the age–depth profile along a flow line from Dome C (DC) to LDC, which is assumed to be stable in time. This means that flow line features such as flow direction and dome location have not changed over the time period considered. The model is constrained by dated radar internal reflecting horizons. Surface velocity measurements are used to determine the flow line and flow tube width, which also allows the model to consider lateral divergence. This new inverse model therefore improves on the methods used by 1D models previously applied to the DC area. This 2.5D model uses a previously developed numerical scheme with the novelty being the inverse methods used to optimise multiple parameters by comparison to radar constraints. By inferring a mechanical ice thickness, the model predicts either the thickness of a basal layer of stagnant ice or a basal melt rate. Results show that the deepest ice at Beyond EPICA Little Dome C (BELDC) originates from around 15 km upstream. The threshold for ice useful for paleoclimatic reconstruction is 20 kyr m−1 (20 000","url":"https://hal.science/hal-05359448v1","contact":"Ailsa Chung, Frédéric Parrenin, Robert Mulvaney, Luca Vittuari, Massimo Frezzotti, Antonio Zanutta, David A Lilien, Marie G P Cavitte","deadline":"2025","source":"HAL","priority":7,"created_at":"2026-06-27T21:42:24.757292","quality_score":88,"quality_reason":"priority=7, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1380,"type":"publication","title":"An enduring, 20-year, multidisciplinary seal-borne ocean sensor research collaboration in the Southern Ocean","institution":"Sydney Institute of Marine Science, Centre d'Études Biologiques de Chizé - UMR 7372, Institute for Marine and Antarctic Studies [Hobart], Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,","description":"Over the last 20 years (2004 to 2025), a French-Australian research and ocean observing collaboration has collected > 400,000 temperature-salinity profiles providing broad coverage within the Indian Sector of the Southern Ocean. The collaboration is the cornerstone of the emerging global Animal-Borne Oceanographic Sensors (AniBOS) network, from which the data are freely available to the operational, ocean and climate research, and public communities. These data are a primary source of information for the study of ocean properties in this remote region, enabling major advances in knowledge of dense water formation, glacial ice shelf melting, frontal structure and recent trends driven by climate change in the Southern Ocean. The data have also provided key observations of biological processes, redefining our understanding of the ecology of seals in the Southern Ocean and providing a detailed picture of how they utilise their dynamic ocean-ice environment. The two-fold delivery of essential oceanographic and ecological observations makes this a flagship program, one which has enabled a step-change in our understanding of coupling between physics and biology. Sustaining the observations delivered by AniBOS is critical within the context of a rapidly changing Southern Ocean, for detecting change and anticipating consequences for these unique coupled systems.","url":"https://hal.science/hal-05172828v1","contact":"Clive Mcmahon, Fabien Roquet, Christophe Guinet, Mark Hindell, Robert Harcourt, Jean-Benoît Charrassin, Sara Labrousse, Ian Jonsen","deadline":"2025","source":"HAL","priority":7,"created_at":"2026-06-27T21:51:45.375730","quality_score":0,"quality_reason":""},{"id":1329,"type":"publication","title":"Analysis of microseismicity in sea ice with deep learning and Bayesian inference: application to high-resolution thickness monitoring","institution":"Institut des Sciences de la Terre, Institut de Physique du Globe de Paris","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,","description":"In the perspective of an upcoming seasonally ice-free Arctic, understanding the dynamics of sea ice in the changing climate is a major challenge in oceanography and climatology. In particular, the new generation of sea ice models will require fine parameterization of sea ice thickness and rheology. With the rapidly evolving state of sea ice, achieving better accuracy, as well as finer temporal and spatial resolutions of its thickness, will set new monitoring standards, with major scientific and geopolitical implications. Recent studies have shown the potential of passive seismology to monitor the thickness, density and elastic properties of sea ice with significantly reduced logistical constraints. For example, human intervention is no longer required, except to install and uninstall the geophones. Building on this approach, we introduce a methodology for estimating sea ice thickness with high spatial and temporal resolutions from the analysis of icequake waveforms. This methodology is based on a deep convolutional neural network for automatic clustering of the ambient seismicity recorded on sea ice, combined with a Bayesian inversion of the clustered waveforms. By applying this approach to seismic data recorded in March 2019 on fast ice in the Van Mijen Fjord (Svalbard), we observe the spatial clustering of icequake sources along the shoreline of the fjord. The ice thickness is shown to follow an increasing trend that is consistent with the evolution of temperatures during t","url":"https://hal.science/hal-04041306v1","contact":"Ludovic Moreau, Léonard Seydoux, Jérôme Weiss, Michel Campillo","deadline":"2023","source":"HAL","priority":7,"created_at":"2026-06-27T21:51:45.375730","quality_score":0,"quality_reason":""},{"id":1389,"type":"publication","title":"Ancient biomolecules from deep ice cores reveal a forested Southern Greenland","institution":"Center for Ancient Genetics, Department of Public Health [Copenhagen], Centre for Comparative Genomics, Max-Planck-Institut für evolutionäre Anthropologie = Max Planck Institute for Evolutionary Anthropology","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,dna,record,holocene,sediments,chronology,instability,pollen,climate","description":"It is difficult to obtain fossil data from the 10% of Earth's terrestrial surface that is covered by thick glaciers and ice sheets, and hence, knowledge of the paleoenvironments of these regions has remained limited. We show that DNA and amino acids from buried organisms can be recovered from the basal sections of deep ice cores, enabling reconstructions of past flora and fauna. We show that high-altitude southern Greenland, currently lying below more than 2 kilometers of ice, was inhabited by a diverse array of conifer trees and insects within the past million years. The results provide direct evidence in support of a forested southern Greenland and suggest that many deep ice cores may contain genetic records of paleoenvironments in their basal sections.","url":"https://hal.science/halsde-00276493v1","contact":"E. Willerslev, E. Cappellini, W. Boomsma, R. Nielsen, M. B. Hebsgaard, T. B. Brand, M. Hofreiter, M. Bunce","deadline":"2007","source":"HAL","priority":7,"created_at":"2026-06-27T21:51:45.375730","quality_score":0,"quality_reason":""},{"id":1327,"type":"publication","title":"Argentière Glacier Characterization by Full Waveforms: Source Inversion as a Preliminary Step","institution":"Laboratoire Jean Kuntzmann, Institut des Sciences de la Terre","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,","description":"The importance of studying glacier behavior and mechanisms has greatly increased in the context of current climate change. In this study, we process seismic data recorded at the surface of the Argentière glacier to characterize its 3D structure. The first step is to characterize the sources responsible for the recorded signals, most of them being icequakes. We start by using the Matched Field Processing method to detect events in the data and spatially localize the icequakes within the glacier. We then build a 3D model of the glacier’s surface topography using digital elevation models. Finally, we invert the focal mechanism and time signature associated with each icequake using an iterative alternating optimization algorithm. The inversion is performed in the elastic approximation and the 3 data components are used. The method is based on a decomposition of the solution of the elastodynamic equations into the derivatives of the Green functions associated with the moment tensor coefficients (characterizing the source mechanism). The results are encouraging: surface waves are generally well reconstructed in the calculated seismograms. Moreover, the estimation of mechanisms yields an interesting result: most icequakes (84%) seem to behave like isotropic sources.","url":"https://hal.science/hal-04792409v1","contact":"Arthur Grange, Romain Brossier, Ludovic Métivier, Philippe Roux, Julien Thurin","deadline":"2024","source":"HAL","priority":7,"created_at":"2026-06-27T21:51:45.375730","quality_score":0,"quality_reason":""},{"id":1346,"type":"publication","title":"Automated delineation and morphometry of unclassified subglacial bedforms","institution":"Laboratoire de Planétologie et Géosciences [UMR_C 6112], Institut de Physique du Globe de Paris, Biogéosciences [UMR 6282]","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,","description":" We designed an automated tool to delineate and analyse the shape of subglacial bedforms using a recently defined land surface parameter, the volumetric obscurance. The tool is based on the assumption that the diversity of subglacial bedform shapes reflects a continuum; therefore, unlike traditional methods, no pre-or post-mapping classification of bedforms is performed. It uses digital elevation models and optical satellite images to generate regional morphological maps (bedform outlines and crestlines) and regional morphometric maps (spatialized statistical analysis of bedform morphometrics). We tested the tool on the ArcticDEM, over a portion of the former Laurentide Ice Sheet bed that displays a wide diversity of bedform shapes (Keewatin Ice Dome, northern Canada). The produced morphological maps are consistent, with a correspondence of approximately 75% on individual bedform outlines, with two reference maps digitized manually by two different glacial geomorphologists. Despite the 25% difference between individual bedform outlines generated automatically and manually, the derived morphometric maps are similar. They can be interpreted in the context of subglacial deformation and hydrology, providing a new potential for palaeoglaciological reconstructions at the ice-sheet scale. The tool was developed in Python and is freely accessible. Here we review the formulations of Holland and Jenkins (1999) for the approximation of heat conduction into ice, utilizing three distinct observed ice temperature profiles. We show that the formulation accounting for constant vertical advection and vertical diffusion of heat into ice best represents the observed ice temperature profiles. Using idealized ocean simulations of a Greenlandic fjord and observed melt rates from Antarctica, we find a difference of up to 28 % (average of 12 %) in melt rates between the different approximations. The term \"water pocket\" describes invisible en-and subglacial water reservoirs that can cause sudden glacial outburst floods. However, there is currently no consensus on its definition and the formation and rupture mechanisms of water pockets remain poorly understood. This study aims to understand the mechanisms behind water pocket outburst floods (WPOFs) from alpine glaciers by analyzing their spatial and temporal distribution, pre-event meteorological conditions, and the glacio-geomorphic features of the glaciers from which the floods originate. To this end, we updated an inventory of known WPOFs in the Swiss Alps to 91 events from 37 individual glaciers. Most WPOFs occurred between June and September, likely linked to meltwater input. Meteorological data indicate anomalously high temperatures during the days preceding most events and heavy precipitation on 25 % of days for which Saharan dust deposits frequently turn alpine glaciers orange and darken their surface. Together with other light-absorbing particles, mineral dust reduces snow albedo, increases snow melt rate, and lowers the surface mass balance of glaciers. Since the surface mass balance drives the evolution of alpine glaciers, assessing the impact of impurities helps to understand their current and future evolution. The location of impurities within the snowpack and their effect on snow albedo can be estimated through physical modelling. In this study, we quantified the impact of dust, taking into account mineral dust and black carbon in snow, on the Argentière Glacier over the period 2019-2022. Our results show that during the three years preceding 2022, the contribution of mineral dust to the annual decrease in surface mass balance was between 0.31-0.45 m w.e., while it reached the double in 2022 with 0.63 m w.e. [0.54, 0.69] (median, [Q10-Q90]), and up to 1.2 m w.e. [0.9, 1.4] at specific locations. The impact of dust in snow was unevenly distributed over the glacier, especially in 2022. The highest simulated impacts occurred where firn layers from previous years were exposed after the total melt of the snowpack of the previ-ous winter. The gravitational redistribution of the snow from avalanches was not taken into account, which can reduce the impact of dust at specific locations. Increasing the modelled scavenging efficiency of black carbon can double the impact of dust alone ","url":"https://hal.science/hal-05345050v1","contact":"Léon Roussel, Marie Dumont, Marion Réveillet, Delphine Six, Marin Kneib, Pierre Nabat, Kévin Fourteau, Diego Monteiro","deadline":"2025","source":"HAL","priority":7,"created_at":"2026-06-27T21:42:24.757292","quality_score":88,"quality_reason":"priority=7, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1324,"type":"publication","title":"Sea Ice Thickness Reconstruction Using Icequake Waveform Inversion and Tomorgraphy","institution":"Institut des Sciences de la Terre","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,tomorgraphy,icequakes,see ice,thickness,seismic waveform,inversion,tomographie,icequakes","description":"Sea ice plays a crucial role in the Earth's climate system, serving both as a driver of and a sensitive indicator for environmental change—particularly in polar and sub-polar regions. This study seeks to improve our understanding of sea ice structure and its temporal variability in response to environmental forces by reconstructing sea ice thickness through seismic waveform inversion and tomography, using both passive and active seismic datasets. The broader goal is to contribute to a better understanding of climate changes.We use forward modeling of seismic wave propagation in sea ice to generate synthetic waveforms, employing the Spectral Element Method (SEM). These synthetic waveforms are then used in an inversion framework that compares them to observed waveforms recorded by seismic receivers deployed on the ice. By minimizing the misfit between synthetic and observed data through a stochastic approach combined with grid search, we estimate ice thickness along source-receiver paths and determine icequake locations. This inversion strategy is applied to both passive and active seismic source data. Once ice thickness estimates are obtained, they are used as input for a second inversion step: seismic tomography. This process yields spatially resolved maps of sea ice thickness.The approach is validated through synthetic tests and applied to several real datasets. The primary dataset, acquired on Lake Vallunden, Svalbard (Norway) between 28 February and 26 March 2019, includes","url":"https://theses.hal.science/tel-05601217v1","contact":"Hooshmand Zandi","deadline":"2025","source":"HAL","priority":7,"created_at":"2026-06-27T21:51:45.375730","quality_score":0,"quality_reason":""},{"id":1306,"type":"publication","title":"Seismic Mapping of Subglacial Hydrology Reveals Previously Undetected Pressurization Event","institution":"Institut des Géosciences de l’Environnement","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,environmental seismology,glacier hydrology,seismology,glaciology,cryoseismology,environmental seismology","description":"Understanding the dynamic response of glaciers to climate change is vital for assessing water resources and hazards, and subglacial hydrology is a key player in glacier systems. Traditional observations of subglacial hydrology are spatially and temporally limited, but recent seismic deployments on and around glaciers show the potential for comprehensive observation of glacial hydrologic systems. We present results from a high-density seismic deployment spanning the surface of Lemon Creek Glacier, Alaska. Our study coincided with a marginal lake drainage event, which served as a natural experiment for seismic detection of changes in subglacial hydrology. We observed glaciohydraulic tremor across the surface of the glacier that was generated by the subglacial hydrologic system. During the lake drainage, the relative changes in seismic tremor power and water flux are consistent with pressurization of the subglacial system of only the upper part of the glacier. This event was not accompanied by a significant increase in glacier velocity; either some threshold necessary for rapid basal motion was not attained, or, plausibly, the geometry of Lemon Creek Glacier inhibited speedup. This pressurization event would have likely gone undetected without seismic observations, demonstrating the power of cryoseismology in testing assumptions about and mapping the spatial extent of subglacial pressurization.","url":"https://insu.hal.science/insu-03706385v1","contact":"Celeste R. Labedz, Timothy C. Bartholomaus, Jason M. Amundson, Florent Gimbert, Marianne S. Karplus, Victor C. Tsai, Stephen A. Veitch","deadline":"2022","source":"HAL","priority":7,"created_at":"2026-06-27T21:51:45.375730","quality_score":0,"quality_reason":""},{"id":1332,"type":"publication","title":"Seismic Monitoring of Permafrost in Svalbard, Arctic Norway","institution":"Laboratoire Chrono-environnement (UMR 6249), Institut für Geowissenschaften","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,resif,epos-france,resif,epos-france","description":"Abstract We analyze data from passive and active seismic experiments conducted in the Adventdalen valley of Svalbard in the Norwegian Arctic. Our objective is to characterize the ambient wavefield of the region and to investigate permafrost dynamics through estimates of seismic velocity variations. We are motivated by a need for early geophysical detection of potentially hazardous changes to permafrost stability. We draw upon several data sources to constrain various aspects of seismic wave propagation in Adventdalen. We use f-k analysis of five years of continuous data from the Spitsbergen seismic array (SPITS) to demonstrate that ambient seismic noise on Svalbard consists of continuously present body waves and intermittent surface waves appearing at regular intervals. A change in wavefield direction accompanies the sudden onset of surface waves when the average temperature rises above the freezing point, suggesting a cryogenic origin. This hypothesis is supported further by our analysis of records from a temporary broadband network, which indicates that the background wavefield is dominated by icequakes. Synthetic Green’s functions calculated from a 3D velocity model match well with empirical Green’s functions constructed from the recorded ambient seismic noise. We use a shallow shear-wave velocity model, obtained from active seismic measurements, to estimate the maximum depth of Rayleigh wave sensitivity to changes in shear velocity to be in the 50–100 m range. We extract ","url":"https://hal.science/hal-03286889v1","contact":"Julie Albaric, Daniela Kühn, Matthias Ohrnberger, Nadège Langet, Dave Harris, Ulrich Polom, Isabelle Lecomte, Gregor Hillers","deadline":"2021","source":"HAL","priority":7,"created_at":"2026-06-27T21:51:45.375730","quality_score":0,"quality_reason":""},{"id":1313,"type":"publication","title":"Seismological insights into englacial and subglacial processes: two case studies from Alpine glaciers","institution":"Géoazur, Laboratory of Hydraulics, Hydrology and Glaciology, Institut des Géosciences de l’Environnement","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,","description":"Englacial and subglacial processes play a critical role in glacier dynamics and stability, yet they are challenging to observe directly. Recent studies have shown that seismology can fill these observational gaps, providing new insights into fundamental cryospheric processes, such as frictional glacier sliding, subglacial water flow, and formation and propagation of cracks and crevasses. Here, we discuss two case studies where seismology reveals new details about mechanical and hydraulic processes in Alpine glaciers: (1) the growth of englacial damage before a break-off event, and (2) temporary reductions in subglacial channel discharge due to sudden changes in frictional conditions within the subglacial channel. First, we analyze seismic data from Switzerland's Eiger hanging glacier before a 15,000 m3 break-off event. We measure seismic source migration by analyzing multiple icequake waveforms using seismic interferometry. Combined with an analytical model based on damage mechanics, our results quantify the englacial damage caused by crevasse extension between unstable and stable ice masses. We then focus on the Rhone lacier in Switzerland, where subglacial hydraulic tremor, driven by turbulent water flow and pressure variations against the subglacial channel bed and walls, acts as a dominant, stable, and coherent noise source. Our analysis reveals sudden hydraulic tremor quieting before and after seismogenic sliding episodes, which is consistent with previous observations. ","url":"https://hal.science/hal-05222759v1","contact":"Malgorzata Chmiel, Nicoletta Caldera, A. Pralong, Florent Gimbert, Martin Funk, Dominik Gräff, Manuela Köpfli, Daniel Farinotti","deadline":"2024","source":"HAL","priority":7,"created_at":"2026-06-27T21:51:45.375730","quality_score":0,"quality_reason":""},{"id":1326,"type":"publication","title":"Spatial and Temporal Variability in Tide‐Induced Icequake Activity at the Astrolabe Coastal Glacier, East Antarctica","institution":"Institut des Géosciences de l’Environnement, Institut Terre Environnement Strasbourg, Ecole et Observatoire des Sciences de la Terre","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,grounding zones,marine-terminating glaciers,glacier,icequake activity,seismic activity","description":"Abstract The grounding zones (GZ) of marine‐terminating glaciers, where ice transitions from grounded to floating, experience strong mechanical changes in response to ocean tides. The spatial and temporal dynamics of these changes remain poorly documented, as they require multi‐scale observations capable of resolving internal ice deformation. Here, we use seismic observations, collected across different years and various scales, coupled with GNSS observations, to evaluate the brittle deformation at the GZ and shear margins of the Astrolabe Glacier (East Antarctica, Terre Adélie). Automatic detection of icequakes reveals that seismic occurrence patterns vary with tides and sensor locations. At a multi‐kilometer scale, we observe and locate numbers of large‐duration magnitude events (average Md around 0.0) associated with shear margins. At a smaller scale (a few hundreds of meters), using a dense array of seismic nodes deployed across the GZ and GNSS observations of vertical ice motion, we capture numerous small‐magnitude events (Md as low as −4.0) with spatial and time occurrences set by tide‐modulated GZ dynamics. At rising tides, seismicity is dominant on the floating part of the glacier, while at falling tides, it is dominant over its grounded part. Based on these observations, we propose a conceptual framework for the dynamics of icequake activity at the glacier GZ, accounting for its three‐dimensional tidal‐induced bending, generating strain rates large enough to induce b","url":"https://hal.science/hal-05339501v1","contact":"Tifenn Le Bris, Guilhem Barruol, Florent Gimbert, Emmanuel Le Meur, Dimitri Zigone, Anuar Togaibekov, Denis Lombardi, Maxime Bès de Berc","deadline":"2025","source":"HAL","priority":7,"created_at":"2026-06-27T21:51:45.375730","quality_score":0,"quality_reason":""},{"id":1345,"type":"publication","title":"Subglacial water amplifies Antarctic contributions to sea-level rise","institution":"Institut des Géosciences de l’Environnement","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,","description":"Antarctica’s contribution to global sea-level rise is deeply uncertain, with subglacial water suspected to play a critical role, yet its impact remains unclear. We demonstrate that water at the base of ice sheets influences sliding behaviour and that its exclusion from models can underestimate sea-level rise projections and delay the predicted onset of tipping points. Here we use an Antarctic Ice Sheet model (Elmer/Ice) to explore how different assumptions about water pressure at the ice base affect sea-level rise projections from 2015 to 2300. Our results indicate that incorporating subglacial water can amplify ice discharge across the Antarctic Ice Sheet by up to threefold above the standard approach, potentially contributing an additional 2.2 metres to sea-level rise by 2300. Notably, a smoothly decreasing basal drag near the grounding line more than doubles grounding line flux by 2300 relative to scenarios where effective pressure is simplified into a spatially constant coefficient. Basin-specific responses vary significantly, with some scenarios advancing tipping points by up to 40 years. These findings underscore the critical need to integrate evolving subglacial hydrology into ice sheet models.","url":"https://hal.inrae.fr/hal-05450904v1","contact":"Chen Zhao, Rupert Gladstone, Thomas Zwinger, Fabien Gillet-Chaulet, Yu Wang, Justine Caillet, Pierre Mathiot, Leopekka Saraste","deadline":"2025","source":"HAL","priority":7,"created_at":"2026-06-27T21:51:45.375730","quality_score":0,"quality_reason":""},{"id":1212,"type":"publication","title":"Surface ice texture mapping of Planpincieux glacier reveals spatial mechanical heterogeneities","institution":"Institut des Géosciences de l’Environnement","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,alpin glacier,ice crystallographic texture,mechanical anisotropy","description":"Crystallographic textures or Crystal Preferred Orientations (CPO) of glacier ice significantly influence its mechanical behavior by transferring mechanical anisotropy from the single-crystal scale to the macroscopic scale. However, their spatial variability and impact on fluidity remain poorly constrained in temperate glaciers. This study presents a detailed mapping of surface crystallographic textures on the Planpincieux Glacier (Mont Blanc Massif, Italy), combining field measurements, surface velocity data, and numerical modeling to assess mechanical heterogeneities. Six sampling zones were analyzed using an Automatic Ice Texture Analyser (AITA), revealing distinct crystallographic texture patterns linked to local strain configurations and boundary conditions. Weak crystallographic textures in zones near the glacier margins and crevasse areas suggest limited viscous deformation, while stronger crystallographic textures indicate deformation under various shear boundary conditions with impact of dynamic recrystallization. The resulting textures are associated with a fluidity enhancement factor reaching up to 2.3 and a fluidity anisotropy up to 5.4. These findings underscore the importance of integrating texture impact into glacier flow models, particularly in temperate environments where recrystallization and complex stress regimes prevail.","url":"https://hal.science/hal-05465250v1","contact":"Thomas Chauve, Line Doucet, Maurine Montagnat, Olivier Gagliardini, Paolo Perret, William Boffelli, Pietro Di Sopra, Luca Mondardini","deadline":"2026","source":"HAL","priority":7,"created_at":"2026-06-27T21:42:24.757292","quality_score":88,"quality_reason":"priority=7, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1218,"type":"publication","title":"Surface mass balance monitoring of an alpine glacier using GNSS Interferometric Reflectometry","institution":"Institut des Géosciences de l’Environnement, Institut des Sciences de la Terre","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,surface mass balance,mountain glaciers,ice and climate,gnss-ir,glacier modelling","description":"Assessing glacier surface mass balance (SMB) is essential for evaluating glacier response to climate change. However, traditional in situ measurement methods are labour intensive and often lack the temporal and spatial resolutions required to fully constrain SMB models. Here, we explore the potential of the Global Navigation Satellite System Interferometric Reflectometry (GNSS-IR) technique which exploits reflected satellite signals to track surface height changes for continuous SMB estimation. Using data from 13 GNSS stations operating between 2019 and 2021 on Glacier d’Argentière (French Alps), we compare GNSS-IR-derived SMB with estimates from snow pits, wooden stakes, continuous ice-melt measurements using a SmartStake device, and a degree-day model. We demonstrate that the GNSS-IR technique can reliably estimate SMB values that closely match independent in situ measurements, while also offering the advantages of spatial integration and long-term time series that capture both snowfall events and snow/ice melt. We show that glacier surface roughness and antenna height, when the glacier is snow-free, strongly influence uncertainties, which can be reduced to as little as 2 cm d −1 using a smoothing filter. Finally, we demonstrate that the GNSS-IR technique can further constrain the degree-day factor, particularly its temporal evolution throughout the ablation season.","url":"https://hal.inrae.fr/hal-05593991v1","contact":"Anuar Togaibekov, Florent Gimbert, Antoine Rabatel, Andrea Walpersdorf","deadline":"2025","source":"HAL","priority":7,"created_at":"2026-06-27T21:42:24.757292","quality_score":88,"quality_reason":"priority=7, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1328,"type":"publication","title":"Surveillance des propriétés de la glace de mer à partir du bruit sismique","institution":"Institut des Sciences de la Terre","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,icequakes,sea ice,thickness,mechanical properties,guided waves,seismic noise,tremblements de glace,bruit sismique","description":"Durant ces quatre dernières décennies, le déclin de l’extension et l’épaisseur moyenne de la glace de mer Arctique s’est accéléré de manière spectaculaire face au réchauffement climatique. Ce déclin est beaucoup plus rapide que celui prédit par les modèles de climat existant. L’évolution de l’étendue de la glace de mer est soumise à des processus thermodynamiques qui sont affectés par des paramètres importants évoluant à un rythme accéléré, tels que les propriétés mécaniques et l’épaisseur de la glace. Bien que les processus physiques expliquant ce déclin soient compris, les modèles actuels de banquise et climatiques ne reproduisent pas clairement les variations observées. Par conséquent, une surveillance continue et précise de ces paramètres est essentielle compte tenu de la nécessité de mettre à jour nos modèles climatiques. L’utilisation de méthodes sismiques pour étudier la glace de mer a longtemps été délaissée malgré leur potentiel pour des estimations très précises des propriétés de la glace. Toutefois, grâce aux rapides progrès technologiques et méthodologiques de la dernière décennie, ces approches ont été récemment reconsidérées.Une partie de cette thèse vise à prouver l’efficacité d’une méthodologie basée sur la mesure des ondes sismiques guidées dans la glace pour estimer son module d’Young, son coefficient de Poisson, sa densité et son épaisseur dans différentes directions en utilisant le bruit sismique ambiant enregistré par un réseau dense de capteurs. Pour ill","url":"https://theses.hal.science/tel-04137571v1","contact":"Agathe Serripierri","deadline":"2023","source":"HAL","priority":7,"created_at":"2026-06-27T21:51:45.375730","quality_score":0,"quality_reason":""},{"id":1320,"type":"publication","title":"Surveillance sismologique des glaciers rocheux : pour mieux contraindre un risque émergent","institution":"Institut des Sciences de la Terre","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,resonance frequency,seismology,noise,éléments finis,fréquence de résonance,sismologie,bruit de fond","description":"Au sein des régions de permafrost de montagne, les glaciers rocheux désignent des formations périglaciaires composées d’un mélange de débris rocheux de granulométrie variable et de matériaux gelés en profondeur. Parmi eux, les glaciers rocheux actifs présentent des vitesses de déplacement de surface de l’ordre du m/an, témoignant d’une dynamique de déformation en profondeur régie par des processus thermo-hydro-mécaniques. Ainsi, leur rôle dans l’apport de sédiments mobilisables en laves torrentielles peut être important, de même que les risques naturels émergents liés à leur déstabilisation. En soutien du suivi cinématique, les méthodes géotechniques et géophysiques permettent d’investiguer en profondeur un glacier rocheux, mais restent ponctuelles et discontinues. En revanche, les méthodes de sismologie environnementale, déjà éprouvées pour la surveillance de glissements de terrain, permettent d’enregistrer des données sismiques continues rendant compte de l’état de la subsurface ; l’objet de cette thèse est donc d’appliquer ces techniques de sismique passive à la surveillance des glaciers rocheux.Deux sites actifs ont donc été instrumentés pendant plusieurs années : le glacier rocheux de Gugla (Valais, Suisse) et celui du Laurichard (Hautes-Alpes, France). À partir des données sismiques recueillies, plusieurs méthodes leur ont été appliquées : corrélation de bruit de fond, microsismicité, analyse spectrale. De façon générale, la variation relative de la vitesse de propagati","url":"https://theses.hal.science/tel-03094893v1","contact":"Antoine Guillemot","deadline":"2020","source":"HAL","priority":7,"created_at":"2026-06-27T21:51:45.375730","quality_score":0,"quality_reason":""},{"id":1386,"type":"publication","title":"The Iso2k database: a global compilation of paleo-δ18O and δ2H records to aid understanding of Common Era climate","institution":"Department of Earth and Planetary Sciences [St Louis], Environnements et Paléoenvironnements OCéaniques, LSU - Department of Geography and Anthropology [Baton Rouge], Center for Marine Environmental Sciences [Bremen]","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,","description":"Reconstructions of global hydroclimate during the Common Era (CE; the past ∼2000 years) are important for providing context for current and future global environmental change. Stable isotope ratios in water are quantitative indicators of hydroclimate on regional to global scales, and these signals are encoded in a wide range of natural geologic archives. Here we present the Iso2k database, a global compilation of previously published datasets from a variety of natural archives that record the stable oxygen (δ18O) or hydrogen (δ2H) isotopic compositions of environmental waters, which reflect hydroclimate changes over the CE. The Iso2k database contains 759 isotope records from the terrestrial and marine realms, including glacier and ground ice (210); speleothems (68); corals, sclerosponges, and mollusks (143); wood (81); lake sediments and other terrestrial sediments (e.g., loess) (158); and marine sediments (99). Individual datasets have temporal resolutions ranging from sub-annual to centennial and include chronological data where available. A fundamental feature of the database is its comprehensive metadata, which will assist both experts and nonexperts in the interpretation of each record and in data synthesis. Key metadata fields have standardized vocabularies to facilitate comparisons across diverse archives and with climate-model-simulated fields. This is the first global-scale collection of water isotope proxy records from multiple types of geolog","url":"https://insu.hal.science/insu-02947242v1","contact":"B. Konecky, Nicholas Mckay, Olga Churakova (sidorova), Laia Comas-Bru, Émilie Dassié, K. Delong, Georgina Falster, Matt Fischer","deadline":"2020","source":"HAL","priority":7,"created_at":"2026-06-27T21:51:45.375730","quality_score":0,"quality_reason":""},{"id":1308,"type":"publication","title":"The RESOLVE project: a multi-physics experiment with a temporary dense seismic array on the Argentière Glacier, French Alps","institution":"Institut des Géosciences de l’Environnement, Institut des Sciences de la Terre","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,","description":"Recent work in the field of cryo-seismology demonstrates that high frequency (>1 Hz) seismic waves provide key constraints on a wide range of glacier processes such as basal friction, surface crevassing or subglacial water flow. Establishing quantitative links between the seismic signal and the processes of interest however requires detailed characterization of the wavefield, which at high frequencies necessitates the deployment of large and particularly dense seismic arrays. Although dense seismic array monitoring has recently become increasingly common in geophysics, its application to glaciated environments remains limited. Here we present a dense seismic array experiment made of 98 3-component seismic stations continuously recording during 35 days in early spring 2018 on the Argentière Glacier, French Alps. The seismic dataset is supplemented with a wide range of complementary observations obtained from ground penetrating radar, drone imagery, GNSS positioning and in-situ measurements of basal glacier sliding velocities and subglacial water discharge. We present first results through conducting spectral analysis, template matching, matched-field processing and eikonal wave tomography. We report enhanced spatial resolution on basal stick slip and englacial fracturing sources as well as novel constraints on the heterogeneous nature of the noise field generated by subglacial water flow and on the link between crevasse properties and englacial seismic velocities. We outline i","url":"https://hal.science/hal-03026304v1","contact":"Florent Gimbert, Ugo Nanni, Philippe Roux, A. Helmstetter, S. Garambois, A. Lecointre, A. Walpersdorf, B. Jourdain","deadline":"2021","source":"HAL","priority":7,"created_at":"2026-06-27T21:51:45.375730","quality_score":0,"quality_reason":""},{"id":1387,"type":"publication","title":"The middle strand of the North Anatolian fault in Iznik region : insights from geomorphology and archeoseismology","institution":"Institut des Sciences de la Terre","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,archeoseismicity,aqueduct,archaeology,geomorphology,active fault,archéosismicité,aqueduc,archéologie","description":"The North Anatolian fault (NAF), a 1000 km-long dextral fault zone is known for its strong seismic hazard. It accommodates the westward motion of Anatolia, relative to Eurasia. In its western part, the NAF splits into three strands, one of which passing south of the Marmara sea and the Iznik lake. This NAF middle strand (MNAF) shows nowadays a very low seismic activity. However, this area has been characterized by a significant earthquake hazard over the last two millennia. Several ancient authors mention the occurrence of more than six destructive earthquakes that impacted Iznik (old Nicaea), which was an important political and religious centre during the Hellenistic and Roman periods. Our study aims to constrain the recent seismic activity on the MNAF in the Iznik area at different time scales through a multidisciplinary approach coupling earth science and archeology.The first goal of this thesis is to develop the study of ancient buildings as archives of the historical seismicity by observing their successive damages and repairs. The city of Nicaea is appropriate for this kind of study as it presents several well preserved ancient buildings that bear traces of numerous repairs. I focus my study on the critical infrastructures for the city such as the 3 km-long protecting walls. This also includes the aqueduct that provided the city with water and is crossed by a segment of active fault, and a Roman basilica recently discovered underwater in the Iznik lake 20 m far from th","url":"https://theses.hal.science/tel-01952234v1","contact":"Yacine Benjelloun","deadline":"2017","source":"HAL","priority":7,"created_at":"2026-06-27T21:51:45.375730","quality_score":0,"quality_reason":""},{"id":1344,"type":"publication","title":"The origin of sinuous ridges in Argyre Planitia: Insights from terrestrial analogues and implications for its hydrology","institution":"Earth-Life Science Institute [Tokyo], Laboratoire de Planétologie et Géosciences [UMR_C 6112]","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,","description":"The Argyre basin, located on the southern highlands, spans over 1500 km wide and is one of the largest impact basins on Mars. Three large valleys drain into Argyre from the southern circumpolar region, whereas the basin is breached at the north and perhaps connected to the Ladon-Morava-Ares outflow system draining into Chryse Planitia. Given its volume and valley connections, this basin played a key role in the global hydrology of early Mars (e.g., Clifford and Parker, 2001; Phillips et al., 2001). Several morphological features indicate that the basin may have contained a lake and/or ice sheet in the past, which could have been fed with meltwater from an ancient south polar ice sheet through three main inlet valleys (e.g., Hiesinger and Head, 2002; Ghatan and Head, 2004). A suite of sinuous ridges in the southern Argyre basin (ASRs)—commonly regarded as eskers—has been interpreted as evidence that an ice sheet once occupied the basin (e.g., Banks et al., 2009; Bernhardt et al., 2013). However, new morphological observations focusing on the context and stratigraphy raise discrepancies with the conventional esker interpretation, leading us to revisit their origin.To assess the origin of these ridges, we first have undertaken detailed morphometric measurements of ASRs and compared them to other glacial and fluvial ridge features on Earth and Mars. We mapped cross-sectional profiles at 1 km intervals along crestlines of ASRs using Context Camera (CTX) images and digital elevatio","url":"https://cnrs.hal.science/hal-05375920v1","contact":"Hiroki Shozaki, Susan Conway, Anna Grau Galofre, Nicolas Mangold, Yasuhito Sekine","deadline":"2025","source":"HAL","priority":7,"created_at":"2026-06-27T21:51:45.375730","quality_score":0,"quality_reason":""},{"id":1336,"type":"publication","title":"Thermally induced icequakes detected on blue ice areas of the East Antarctic ice sheet","institution":"Institut de Physique du Globe de Paris, Centro de Estudos do Ambiente e do Mar = Centre for Environmental and Marine Studies [Aveiro]","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,seismology,ice temperature,ice rheology,blue ice,antarctic glaciology","description":"Over a year of seismic observations, ∼5000 short duration icequakes were detected by a permanent broadband station installed at the Princess Elisabeth base, located ∼180 km inland in eastern Dronning Maud Land, East-Antarctica. Icequake detection via seismic waveform pattern recognition indicates the presence of two dominating clusters of events, totalizing ∼1500 icequakes. The corresponding icequake locations point towards two distinct zones of outcropping blue ice areas (BIAs) located respectively at 4 and 1 km from the seismic station, both on the leeward side of a nunatak protruding through the ice sheet. The temporal occurrence of these icequakes suggests a close genetic link with thermal contraction of ice caused by significant surface cooling controlled, in summer by variations in diurnal solar radiation and in winter by strong cooling during cold katabatic regimes. Further analysis demonstrates the dependence of these icequakes on the absolute surface temperature and on its temporal change. Besides providing information on the ice fracture mechanics and rheology, investigations of thermal icequakes may be regarded as a ground-based proxy for the monitoring of the thermal state of BIAs, and characterization of ice-sheet ablation zones.","url":"https://hal.science/hal-02289922v1","contact":"Denis Lombardi, Irina V Gorodetskaya, Guilhem Barruol, Thierry Camelbeeck","deadline":"2019","source":"HAL","priority":7,"created_at":"2026-06-27T21:51:45.375730","quality_score":0,"quality_reason":""},{"id":1321,"type":"publication","title":"Towards mechanical modeling of rock glaciers from modal analysis of passive seismic data","institution":"Institut des Sciences de la Terre, Environnements, Dynamiques et Territoires de Montagne, CANTON DU VALAIS SION CHE","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,","description":"<p>Among mountainous landforms, rock glaciers are mostly abundant in periglacial areas, as tongue-shaped heterogeneous bodies. By measuring physical properties sensitive to useful hydro-mechanical parameters of the medium, a wide range of geophysical methods provides interesting tools to characterize and monitor rock glaciers at large scale<sup>(1)</sup>. However, the need of high resolution temporal monitoring reduces the choice of such methods.</p><p>Passive seismic monitoring systems have the potential to overcome these difficulties, as recently shown on the Gugla rock glacier<sup>(2)</sup>. Indeed, seismological networks provide continuous recordings of both seismic ambient noise and microseismicity. From spectral analysis, we track resonance frequencies and modal parameters that are directly linked to elastic properties of the system, which evolve according to its rigidity and its density<sup>(3)(4)</sup>. Here, we propose to evaluate the potential of this methodology on two rock glaciers (Laurichard and Gugla) located in the Alps, at elevations where climatic forcing influences their internal structures and consequently their dynamics.</p><p>For both sites, we succeed in tracking and monitoring resonance frequencies of vibrating modes during several years. These frequencies show seasonal variations, indicating a freeze-thawing effect on elastic properties of the structure.</p><p>Assuming vibra","url":"https://hal.science/hal-03083937v1","contact":"Antoine Guillemot, Laurent Baillet, Stéphane Garambois, Xavier Bodin, Éric Larose, Agnès Helmstetter, Raphaël Mayoraz","deadline":"2020","source":"HAL","priority":7,"created_at":"2026-06-27T21:51:45.375730","quality_score":0,"quality_reason":""},{"id":1214,"type":"publication","title":"Tracking extinct glaciers in GLIMS","institution":"Institut des Géosciences de l’Environnement","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,glacier hydrology glacier mass balance glacier mapping glacier monitoring,glacier monitoring,glacier mapping,glacier mass balance,glacier hydrology","description":"Global Land Ice Measurements from Space (GLIMS), an initiative to build and distribute a database of global glacier data, has recently begun to track glaciers that have recently disappeared. GLIMS provides a definition of “extinct” glaciers for our community, and the final determination of extinction is left to local experts. There are currently 181 glaciers in the GLIMS Glacier Database that are marked as “extinct”, though we recognize that there have been many more reported in the literature. GLIMS welcomes more submissions to make the list more complete.","url":"https://hal.inrae.fr/hal-05593984v1","contact":"Bruce H Raup, Liss Marie Andreassen, Dominic Boyer, Cymene Howe, Mauri Pelto, Antoine Rabatel","deadline":"2025","source":"HAL","priority":7,"created_at":"2026-06-27T21:42:24.757292","quality_score":88,"quality_reason":"priority=7, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1316,"type":"publication","title":"Uncertainty analysis of digital elevation models by spatial inference from stable terrain","institution":"Laboratoire d'études en Géophysique et océanographie spatiales, Versuchsanstalt für Wasserbau, Hydrologie und Glaziologie, Institut des Géosciences de l’Environnement","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,","description":"The monitoring of Earth's and planetary surface elevations at larger and finer scales is rapidly progressing through the increasing availability and resolution of digital elevation models (DEMs). Surface elevation observations are being used across an expanding range of fields to study topographical attributes and their changes over time, notably in glaciology, hydrology, volcanology, seismology, forestry, and geomorphology. However, DEMs frequently contain large-scale instrument noise and varying vertical precision that lead to complex patterns of errors. Here, we present a validated statistical workflow to estimate, model, and propagate uncertainties in DEMs. We review the state-of-the-art of DEM accuracy and precision analyses, and define a conceptual framework to consistently address those. We show how to characterize DEM precision by quantifying the heteroscedasticity of elevation measurements, i.e., varying vertical precision with terrain- or sensor-dependent variables, and the spatial correlation of errors that can occur across multiple spatial scales. With the increasing availability of high-precision observations, our workflow based on independent elevation data acquired on stable terrain can be applied almost anywhere on Earth. We illustrate how to propagate uncertainties for both pixel-scale and spatial elevation derivatives, using terrain slope and glacier volume changes as examples. We find that uncertainties in DEMs are largely underestimated in the literature, ","url":"https://hal.science/hal-03719624v1","contact":"Romain Hugonnet, Fanny Brun, Etienne Berthier, Amaury Dehecq, Erik Schytt Mannerfelt, Nicolas Eckert, Daniel Farinotti","deadline":"2022","source":"HAL","priority":7,"created_at":"2026-06-27T21:51:45.375730","quality_score":0,"quality_reason":""},{"id":1372,"type":"publication","title":"Weddell seals foraging ecology in relation to interannual variability in sea ice conditions between 2006 and 2024 in Terre Adélie, East Antarctica","institution":"Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,foraging ecology,polar predator,sea ice,environmental variability,diving behaviour,biotelemetry,glace de mer,prédateur polaire","description":"In marine environments, where resources are distributed heterogeneously, predators rely on environmental cues to locate prey aggregations and optimise energy intake through foraging. Variability in local conditions thus influences prey distribution and availability, which are reflected in predators' foraging behaviour and spatial patterns. Studying this behaviour and its variability offers insights into environmental drivers, prey dynamics, and broader ecosystem processes. In polar regions, predators depend on sea ice not only as a platform for breeding, moulting, and resting but also as a crucial foraging habitat. Sea ice supports an entire ecosystem both at the ocean/ice interface and underneath. The structure, extent, and seasonal dynamics of Antarctic sea ice are central to Southern Ocean processes and ecology. Sea ice influences the timing of phytoplankton blooms, with cascading effects throughout the food web. Abrupt episodic events like glacier calvings can profoundly reshape the sea ice landscape, altering bloom timing and redistributing key habitats. These include predator haul-out platforms, ocean access points for land-based species, benthic habitats subject to iceberg scouring, under-ice feeding and nursery zones for fish, and sea ice algae growth areas. Weddell seals (Leptonychotes weddellii) are the only marine mammal fully dependent on landfast ice year-round. From 2006 to 2024, the at-sea movements and diving behaviour of female Weddell seals were studied usin","url":"https://theses.hal.science/tel-05599959v1","contact":"Adélie Antoine","deadline":"2025","source":"HAL","priority":7,"created_at":"2026-06-27T21:51:45.375730","quality_score":0,"quality_reason":""},{"id":1337,"type":"publication","title":"Where do we want the glaciological community to be in 2073? Equality, diversity and inclusion challenges and visions from the 2023 Karthaus Summer School","institution":"Institut des Géosciences de l’Environnement","country":"France / Europe","city":"","latitude":null,"longitude":null,"tags":"hal,publication,france,open archive,applied glaciology community edi ice and climate ice-sheet modelling,ice-sheet modelling,ice and climate,edi,community,applied glaciology","description":"Despite the increased awareness and action towards Equality, Diversity and Inclusion (EDI), the glaciological community still experiences and perpetuates examples of exclusionary and discriminatory behavior. We here discuss the challenges and visions from a group predominantly composed of early-career researchers from the 2023 edition of the Karthaus Summer School on Ice Sheets and Glaciers in the Climate System. This paper presents the results of an EDI-focused workshop that the 36 students and 12 lecturers who attended the summer school actively participated in. We identify common threads from participant responses and distill them into collective visions for the future of the glaciological research community, built on actionable steps toward change. In this paper, we address the following questions that guided the workshop: What do we see as current EDI challenges in the glaciology research community and which improvements would we like to see in the next fifty years? Contributions have been sorted into three main challenges we want and need to face: making glaciology (1) more accessible, (2) more equitable and (3) more responsible.","url":"https://hal.inrae.fr/hal-05450715v1","contact":"Lena Nicola, Rebekka Frøystad, Antonio Juarez-Martinez, Maxence Menthon, Ana Carolina Moraes Luzardi, Katherine A Turner, Sally F Wilson, Nanna B Karlsson","deadline":"2025","source":"HAL","priority":7,"created_at":"2026-06-27T21:51:45.375730","quality_score":0,"quality_reason":""},{"id":1031,"type":"publication","title":"40 Years of AMS at the Technical University of Munich","institution":"Technical University of Munich","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,technical university,accelerator mass spectrometry,nuclear transmutation,library science,nuclear physics,manhattan project","description":"Abstract In this review we describe the Accelerator Mass Spectrometry activities in Munich and some of the achievements of the past 40 years. These comprise subjects in geology, technetium distribution in the environment, dosimetry and atomic bomb survivors, input into the Solar System from close and recent supernovae, the search for primordial superheavy nuclei, the search for violations of the Pauli exclusion principle as well as the determination of the half-life of beryllium-10, a cosmogenic isotope extensively used for geology and other sciences.","url":"https://doi.org/10.1007/s10967-026-10992-z","contact":"G. Korschinek, T. Faestermann","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":334,"type":"publication","title":"A 3D passive ring gyroscope for seismology","institution":"arXiv","country":"International","city":"","latitude":null,"longitude":null,"tags":"arxiv,publication,preprint","description":"In seismology and related fields, the measurement of rotation in all three spatial dimensions is essential to complement the observation of translations. Access to all six degrees of freedom allows for full reconstruction of seismic wavefields and improves the understanding of complex ground motion during seismic events. In this regard, Sagnac interferometers in the form of large active ring laser systems have demonstrated remarkable performance. So-called passive ring gyroscopes offer the potential to bypass some of the limitations of active ring lasers and could represent a promising complement to existing sensor technology. Here, we present a prototype of a transportable three dimensional free-space passive ring gyroscope, reaching a sensitivity in the micro rad/s/sqrt(Hz) regime in all spatial dimensions. We demonstrate the sensor performance by reconstructing the rotational components of a simulated seismic event.","url":"http://arxiv.org/abs/2606.19976v1","contact":"","deadline":"2026-06-18T09:12:36Z","source":"arXiv","priority":5,"created_at":"2026-06-27T21:27:28.763349","quality_score":73,"quality_reason":"priority=5, has_url, trusted_source, good_description, detailed_description, good_tags"},{"id":405,"type":"publication","title":"A Framework for Structural-Collapse-Sensitive Ground-Motion Identification Based on Unsupervised Clustering and Explainable Ensemble Learning","institution":"Kunming University of Science and Technology, Yunnan Agricultural University, Yunnan Earthquake Prevention and Disaster Reduction","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,interpretability,cluster analysis,computer science,artificial intelligence,random forest,feature selection","description":"To address the small ATC-63 record set for collapse-oriented motion selection and the limited interpretability of data-driven approaches, this study proposes a framework for identifying structural-collapse-critical ground motions. Using 5074 records from the PEER NGA-West2 database, we applied STA/LTA event detection and extracted multi-source features. A Gaussian mixture model (GMM) was then used to perform unsupervised clustering and identify four physically interpretable groups. LightGBM, XGBoost, and Random Forest were employed to test the separability of the cluster labels, with all three models achieving F1 scores above 0.89 and LightGBM reaching an accuracy of about 93%. SHAP-based feature-importance analysis was used at the model level to clarify feature contributions and improve interpretability. Cluster 2 exhibits markedly higher relative seismic energy, stronger time-domain variability, and more dominant frequencies, forming a typical strong-motion hazard signature. For external engineering verification, 22 ATC-63 far-field records were mapped onto the full dataset to examine cluster-level enrichment and coverage. Cluster 2 shows significant enrichment in engineering markers and high coverage and is therefore identified as the collapse-sensitive phenotype cluster (COP). Overall, the framework provides a technical basis for ground-motion selection in collapse assessment, fragility analysis, and design evaluation.","url":"https://doi.org/10.3390/buildings16040820","contact":"Xinyu Zhao, Wen Pan, YE Liao-yuan","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":357,"type":"publication","title":"A Low-PAPR, Synchronization-Robust Non-Coherent Grassmannian Modulation for Optical Communications","institution":"arXiv","country":"International","city":"","latitude":null,"longitude":null,"tags":"arxiv,publication,preprint","description":"Non-coherent Grassmannian (unitary space-time) signaling detects on the received subspace, which is invariant to a branch-side (polarization or mode-coupling) rotation and to a phase that is constant over the coherence block. It therefore needs no carrier-phase or polarization recovery within the block and is robust to phase noise when the per-block phase drift is small, while a multi-branch (polarization or spatial) front end harvests diversity without channel estimation or pilots. However, the Grassmannian-constellation literature usually assumes a distortion-free, linear channel and transmitter and already-acquired symbol timing. This paper closes both gaps while reusing off-the-shelf Grassmannian packings. First, we impose a constant-modulus (low peak-to-average-power-ratio, PAPR) constraint on the constellation and quantify the PAPR/chordal-distance trade-off: a constant-modulus design lowers the 0.1% PAPR from 6.1 dB (unconstrained) to 3.6 dB -- 1.6 dB below 16-QAM (5.2 dB) -- easing the optical modulator linear range and the fiber Kerr-nonlinearity penalty, at a ~1.8 dB cost in high-SNR coding gain. Second, we derive a phase-blind subspace timing-error detector (TED) that ex","url":"http://arxiv.org/abs/2606.26464v1","contact":"","deadline":"2026-06-24T23:59:13Z","source":"arXiv","priority":5,"created_at":"2026-06-27T21:27:28.763349","quality_score":73,"quality_reason":"priority=5, has_url, trusted_source, good_description, detailed_description, good_tags"},{"id":1097,"type":"publication","title":"A New Model Perspective: TheImpact of Enso and the Rising Sea Level Trend in Vietnam","institution":"The State Bank of Vietnam, Banking Academy of Vietnam","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,sea level,tide gauge,environmental science,el niño southern oscillation,sea level rise,climatology","description":"Publication from OpenAlex. Authors: Thi Quynh Nhung Le. Year: 2026","url":"https://doi.org/10.21203/rs.3.rs-9702351/v1","contact":"Thi Quynh Nhung Le","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":68,"quality_reason":"priority=6, has_url, trusted_source, good_tags, has_contact_or_authors"},{"id":697,"type":"publication","title":"A Non-Reference Diffusion-Based Restoration Framework for Landsat 7 ETM+ SLC-off Imagery in Antarctica","institution":"OpenAlex","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,remote sensing,geology,satellite imagery,limiting,pixel,computer science","description":"Acquiring usable optical imagery in Antarctica is inherently challenging due to prolonged polar nights and frequent cloud cover. Landsat provides the longest and most continuous optical observations and constitutes one of the most important remote sensing data sources for Antarctic studies. However, the scan-line corrector (SLC) failure in 2003 resulted in approximately 22% missing pixels in Landsat 7 ETM+ SLC-off imagery, severely limiting its usability. Unlike many non-polar environments, Antarctic surfaces undergo rapid and substantial changes, which makes it difficult to obtain reliable reference imagery and reduces the applicability of conventional reference-based gap-filling methods. To address this challenge, we propose DiffGF, a non-reference diffusion-based framework for restoring Landsat 7 SLC-off imagery without requiring any external reference data. DiffGF adopts a two-stage design consisting of a latent-space diffusion process and a pixel-space refinement. A dedicated Antarctic dataset, SLCANT, is constructed for training and evaluation. Quantitative and qualitative results demonstrate that DiffGF restores Antarctic SLC-off imagery with high fidelity. Its practical value is further examined through a downstream crevasse segmentation application. The results suggest that DiffGF provides a useful approach for exploiting Landsat 7 SLC-off archives in Antarctica, enabling the extraction of valuable information from historical records and supporting related Antarctic ","url":"https://openalex.org/W7162149888","contact":"Leyue Tang, Jonathan Louis Bamber, Gang Qiao, Yuanhang Kong","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":569,"type":"publication","title":"A Scoping Review of Digital Twins Across Environmental and Territorial Applications","institution":"Università Iuav di Venezia, Robert Bosch (Germany)","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,environmental resource management,regional science,diversification (marketing strategy),position (finance),economic geography,conceptual framework","description":"Digital twin (DT) technology has expanded far beyond its industrial origins, increasingly finding application across environmental and territorial domains. This review provides a structured mapping of DT deployments at environmental and territorial scales over the period 2020–2025, examining 117 peer-reviewed publications (109 applied studies and 8 review articles) through a structured 16-parameter classification framework. The review traces three major conceptual shifts in the DT paradigm: from industrial assets to living entities, from discrete systems to Earth-scale representations, and from closed deterministic models to ecological and systemic frameworks, as reflected in the emergence of ecological digital twins (EcoDTs), environmental digital twins (EDTs), and territorial digital twin (TDT) definitions. The results reveal a clear growth trajectory in DT applications across themes, with urban systems as the most consolidated application domain, and progressive diversification into marine, coastal, forestry, river/lake, and Earth system applications from 2022 onward. Institutional actors dominate production in this space, aligned with European flagship initiatives such as Destination Earth (DestinE) and the European Digital Twin of the Ocean (EDITO). The findings position and expand the notion of territorial digital twins as an evolving paradigm, underscoring both the momentum generated by EU digital and environmental policy and the need for integrated tools to answer and","url":"https://doi.org/10.3390/digital6030053","contact":"Letizia Artioli, Giovanni Borga, Pietro Costa, Federica D’Acunto, Filippo Iodice","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":700,"type":"publication","title":"A basin-scale mapping method for crevasse depth using ICESat-2: a case study on Greenland's Sermeq Kujalleq (Jakobshavn Isbræ)","institution":"Institute of Geodesy and Geophysics, University of Chinese Academy of Sciences, University of St Andrews, University of Sheffield, Wuhan University, State Key Laboratory of Information Engineering in Surveying Mapping and Remote Sensing","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,crevasse,geology,geomorphology,remote sensing,meltwater,ice sheet","description":"Abstract. Surface crevasses across the Greenland Ice Sheet remain a major source of uncertainty in understanding mass loss processes, including calving, ice flow, and meltwater routing. Most previous studies have primarily focused on the two-dimensional characteristics of surface crevasses on the Greenland Ice Sheet, measurement of crevasse depth, especially from catchment to ice-sheet scale, is limited, thereby limiting our ability to quantify their impact on ice-sheet stability and surface hydrology. The ICESat-2 ATL03 data (0.7 m resolution) provide an unprecedented opportunity to measure crevasse depths, yet large-scale applications are hindered by challenges such as massive data volume and noises. Here, we develop an automated and efficient ICESat-2 method for crevasse depth estimation that rapidly identifies crevassed regions using a novel roughness index, retrieves signal photons via a similarity-based weighted density approach, and extracts crevasses for depth estimation using a local extrema method. A total of 18,775 crevasse locations were detected from 2,286 beams on Sermeq Kujalleq in 2019. The average crevasse depth is 7.20 ± 0.03 m, with depth maxima occurring at approximately 20 km and 10 km inland in the south and north ice streams, respectively. Crevasses in the northern ice stream are mainly distributed below 600 m a.s.l, whereas those in the southern ice stream predominantly occur below 900 m a.s.l. Compared to IceBridge ATM data, the RMSE of crevasse depth","url":"https://doi.org/10.5194/egusphere-2026-2598","contact":"Ruijie Chang, Xi Lu, Ran Huang, Andrew J. Sole, Stephen J. Livingstone, Zhen Dong, Liming Jiang, Hansheng Wang","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1179,"type":"publication","title":"A classroom activity on global glacier mass balance and glacier climate feedback","institution":"Universidade do Porto, University of Coimbra, Complejo Hospitalario Universitario de Santiago","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,glacier,climate change,balance (ability),discipline,science education,global warming","description":"Abstract This article presents a didactic sequence for upper secondary physics that integrates climate change education through the analysis of glacier mass balance. Using authentic data from the World Glacier Monitoring Service (1980–2023), it is proposed that students engage in a collaborative inquiry and mathematical modelling to explore the accelerated decline of global glacier ice mass. The activity introduces climate feedback mechanisms through a simplified model that students fit to real observational data. By comparing model predictions with measurements, students discover that glacier mass loss acceleration results from positive feedback processes that amplify the effects of atmospheric warming, as quantified through an effective feedback coefficient. Data analysis enables students to project the complete melting of non-Greenland and non-Antarctic glaciers within a century. The pedagogical approach combines authentic scientific data, collaborative modelling, and socially relevant contexts to develop both disciplinary knowledge and transversal competences. The activity is designed for practical implementation using standard computational tools and publicly accessible data, contributing to scientific literacy and informed engagement with contemporary environmental challenges.","url":"https://doi.org/10.1088/1361-6552/ae7007","contact":"M. A. Salgueiro da Silva, Bento Cavadas, T. M. Seixas","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":797,"type":"publication","title":"A community vision for next-generation bed mapping in Antarctica","institution":"Norwegian Polar Institute, University of Edinburgh, University of Exeter","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,drone,geology,antarctic ice sheet,earth science,oceanography,ice sheet","description":"Antarctic bed mapping underpins our understanding of ice-sheet stability, grounding-line retreat and future sea-level rise. Detailed geomorphological and geophysical knowledge, integrated with geological characteristics, reveals long-term processes such as erosion, sediment transport to the ocean and contributions to global geochemical cycles. Despite major advances in radar surveys, large regions of the Antarctic Ice Sheet remain poorly constrained. A side meeting held on 8 May 2025, immediately after the Royal Society's Theo Murphy Meeting on Next Generation Ice-sheet Bed Measurements, gathered international experts to identify priorities for advancing coordinated surveys, data integration and open infrastructure. These discussions, timely as the community prepares for the fifth International Polar Year (IPY5; 2032-2033), emphasized harmonized survey design, closer integration with modelling and remote-sensing communities, improved data standards and archiving, and implementation of emerging technologies such as swath radar, drone and artificial intelligence-assisted data interpretations. Together, they highlight both the urgency and the opportunity to build an internationally coherent framework for next-generation Antarctic bed measurements. This article is part of the Theo Murphy meeting issue 'Next generation ice-sheet bed measurements'.","url":"https://doi.org/10.1098/rsta.2025.0372","contact":"Kenichi Matsuoka, Robert G. Bingham, Helen Millman, Martin Siegert","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1288,"type":"publication","title":"A comprehensive review of seismic resilience of communication systems: An earthquake engineering perspective","institution":"Reliability Engineering & System Safety","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":"Crossref publication metadata. Journal: Reliability Engineering & System Safety. Authors: Changhai Zhai, Fan Li, Chenxi Mao, Hao Qin, Zeqian Wu. Year: 2026.","url":"https://doi.org/10.1016/j.ress.2026.112829","contact":"Changhai Zhai, Fan Li, Chenxi Mao, Hao Qin, Zeqian Wu","deadline":"2026","source":"Crossref","priority":6,"created_at":"2026-06-27T21:51:40.076393","quality_score":0,"quality_reason":""},{"id":245,"type":"publication","title":"A diagnostic framework for tidal signal recovery under diurnal environmental aliasing: application to a fiber-optic and seismic deployment on Astrolabe Glacier, East Antarctica","institution":"Centre National de la Recherche Scientifique, Université de Strasbourg, Institut des Géosciences de l'Environnement","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,geology,geophone,induced seismicity,sea level,glacier,sampling (signal processing)","description":"Icequake seismicity on coastal glaciers is thought to be controlled by ocean tidal forcing, but short deployments make this difficult to verify: in diurnal tidal environments, wind, temperature, and atmospheric pressure all vary on approximately 24-hour cycles near-indistinguishable in period from the K1 tidal constituent (23.93 hours). This near-collinearity means that naïve tidal analysis on a short record risks measuring the diurnal environmental cycle rather than a physical tidal response, an aliasing problem that has not, to our knowledge, been formally characterised or addressed in the seismological literature. Without a framework to separate the two, short-record analyses cannot determine whether an observed correlation between tidal height and seismicity rate is physical or spurious. A previous deployment on Astrolabe Glacier (Le Bris et al., 2025) identified a tidal phase signal but, suspecting that wind interfered with seismic detection, restricted their analysis to low-wind periods rather than systematically characterising the environmental confounders or quantifying how much of the observed signal could be attributed to aliasing rather than tidal forcing.The January 2024 SeisAdelice experiment on Astrolabe Glacier, Adélie Land, East Antarctica served as the development and testing site for a deconfounding framework targeting this problem. The network comprised 37 three-component seismic nodes concentrated within a 2 × 0.6 km strip across the glacier's grounding li","url":"https://doi.org/10.5194/egusphere-gc14-fibreoptic-8","contact":"Alessia Maggi, Cassandra Batista, Dimitri Zigone, Tifenn Le Bris, Guilhem Barruol","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:18:32.932503","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1106,"type":"publication","title":"A high-resolution Sentinel-2 dataset of Antarctic coastal snow algal dynamics (2018–2025) generated using cloud-scale parallel processing","institution":"Chinese Academy of Sciences, Aerospace Information Research Institute, University of Chinese Academy of Sciences, Beihang University","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,environmental science,snow,remote sensing,parallel processing,meteorology,climatology","description":"Antarctic coastal snow algal blooms are ecologically important, but remain poorly documented at continental scales because of logistical constraints on field observations. Here, we present a high-resolution, multi-season Sentinel-2 dataset of Antarctic coastal snow algal blooms covering the western Antarctic coastal margin 2018–2025. The dataset was generated using all available Sentinel-2 Level-2A observations acquired during the austral summer within a 100 km inland coastal buffer, processed through a hybrid workflow combining cloud-based preprocessing on Google Earth Engine with parallelized server-side analysis. Seasonal median composites at 10 m spatial resolution were used to calculate the chlorophyll-sensitive index (IB4) for green snow algae detection. IB4 values were converted into algal cell concentration estimates using a published field-calibrated model, followed by spectral, spatial, and concentration-based filtering to remove false positives. To our knowledge, this study produced the first spatially continuous seven-year Sentinel-2-derived trend dataset for Antarctic coastal snow algae by quantifying pixel-level temporal trends using a modified Mann–Kendall test. The open dataset includes seasonal maps of algal presence (IB4), estimated cell concentration, and robust trend metrics. This resource supports studies of cryosphere–biosphere interactions, albedo feedback, and climate sensitivity. The dataset is publicly available in ScienceDB (https://doi.org/10.57760","url":"https://doi.org/10.1080/20964471.2026.2688641","contact":"Barjeece Bashir, Dong Liang, Rong Cai, Faisal Mumtaz, Lingyi Kong, Yue Wang, Adeel Ahmad","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":353,"type":"publication","title":"A hybrid IFENN solver for generalizable modeling of phase-field fracture initiation and propagation","institution":"arXiv","country":"International","city":"","latitude":null,"longitude":null,"tags":"arxiv,publication,preprint","description":"In this paper we demonstrate how the Integrated Finite Element Neural Network (IFENN) framework can effectively model the entire evolution of phase-field fracture, including the initiation and propagation stage, across generalizable geometries. IFENN is a hybrid scheme for coupled computational mechanics problems, tightly coupling a standard FEM solver (mechanical equilibrium) with a pre-trained neural network (coupled field). In this work, the phase-field diffusion equation is approximated with: i) a DeepONet architecture with Kolmogorov-Arnold networks in the trunk and branch (DeepOKAN) for the initiation stage, and ii) a Convolution Neural Network (CNN) for the propagation stage. Both networks are trained only once, on a benchmark geometry, using a purely physics-informed approach based on the maximum strain energy and the phase-field variable. The training process utilizes an extremely small number of training increments and only a limited number of Gauss points that are strategically sampled from the fracture process zone. These features enable a substantial decrease of the offline training cost. To address the extrapolation of the DeepOKAN predictions in regions away from the","url":"http://arxiv.org/abs/2606.27177v1","contact":"","deadline":"2026-06-25T15:43:19Z","source":"arXiv","priority":5,"created_at":"2026-06-27T21:27:28.763349","quality_score":73,"quality_reason":"priority=5, has_url, trusted_source, good_description, detailed_description, good_tags"},{"id":1269,"type":"publication","title":"A hybrid PEMFC-ICE system powered by on-site ammonia decomposition: techno-economic and environmental optimization considering waste heat recovery","institution":"Fuel","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":"Crossref publication metadata. Journal: Fuel. Authors: Jiang-Hai Xu, Shuo Yuan, Zi-Zhang Zhan, Yi-Yu Chen, Yuan-Li Liu, Tai-Ming Huang, Zhong-Min Wan, Xiao-Dong Wang. Year: 2027.","url":"https://doi.org/10.1016/j.fuel.2026.140070","contact":"Jiang-Hai Xu, Shuo Yuan, Zi-Zhang Zhan, Yi-Yu Chen, Yuan-Li Liu, Tai-Ming Huang, Zhong-Min Wan, Xiao-Dong Wang","deadline":"2027","source":"Crossref","priority":6,"created_at":"2026-06-27T21:51:40.076393","quality_score":0,"quality_reason":""},{"id":367,"type":"publication","title":"A modified Euler-Maruyama method to simulate a one-dimensional sticky diffusion","institution":"arXiv","country":"International","city":"","latitude":null,"longitude":null,"tags":"arxiv,publication,preprint","description":"A sticky diffusion is a process that can stick to and detach from a lower-dimensional boundary. A challenge in simulating such a process is in capturing the change in dimension in a dynamically consistent way. We introduce a numerical algorithm to simulate a one-dimensional sticky diffusion, which sticks to and detaches from a point. Our method is a simple modification of the standard Euler-Maruyama scheme, which chooses with some probability between a reflected Euler-Maruyama update and a jump to the sticky point. We show how to choose this probability to be consistent with the generator of the desired dynamics, and we prove that our scheme converges weakly to a sticky diffusion with order 1.","url":"http://arxiv.org/abs/2606.27259v1","contact":"","deadline":"2026-06-25T16:44:07Z","source":"arXiv","priority":5,"created_at":"2026-06-27T21:27:28.763349","quality_score":73,"quality_reason":"priority=5, has_url, trusted_source, good_description, detailed_description, good_tags"},{"id":1238,"type":"publication","title":"A multi-scale state-space expert hybrid network algorithm for acoustic-based glacier calving event detection","institution":"Signal Processing","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":"Crossref publication metadata. Journal: Signal Processing. Authors: Yankun Chen, Yichen Duan, Zhiyuan Li. Year: 2026.","url":"https://doi.org/10.1016/j.sigpro.2026.110703","contact":"Yankun Chen, Yichen Duan, Zhiyuan Li","deadline":"2026","source":"Crossref","priority":6,"created_at":"2026-06-27T21:51:40.076393","quality_score":0,"quality_reason":""},{"id":663,"type":"publication","title":"A novel database of Antarctic meteorological extremes over key ice shelves during 1995–2023","institution":"University of Lincoln, British Antarctic Survey, University of Oxford, Institute of Marine Geology and Geophysics, University of Sheffield, University of Liège, Danish Meteorological Institute","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,climatology,sea ice,environmental science,anomaly (physics),climate model,cryosphere","description":"Abstract. The climate of Antarctica is showing increasing signs of being impacted by the warming trend in global temperatures, which has potential to result in accelerated break up of key ice shelves, which would contribute to global sea level rise. Here, we present a novel database of Antarctic extreme weather events over a selection of key ice shelves (Larsen, George VI, Wilkins, Abbot, Thwaites, Totten, Amery, Lazarev), using simulations from four regional climate models (RCMs: RACMO2, HCLIM, MetUM and MAR), driven by the ERA5 reanalysis, examining surface air temperature, precipitation, wind and surface pressure. In addition, we examine trends in the frequency of extreme events above or below specified thresholds (5th, 10th, 50th, 90th and 95th percentiles) and spatial atmospheric circulation and temperature anomaly patterns over Antarctica that are commonly associated with extreme events over key ice shelves. The RCM simulations have been compared with station observations close to the ice shelves, and we developed regressions to estimate simulated values during periods when only one or two of the RCMs were available.","url":"https://doi.org/10.5194/egusphere-2026-2270","contact":"Ian Simpson, Edward Hanna, Ryan S. Williams, Linh Luu, Andrew Orr, J.C. Jones, X Fettweis, Jose Abraham Torres Alavez","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1285,"type":"publication","title":"A physics-informed multivariate ensemble framework for seismic fragility of shield tunnels with heteroscedastic and non-Gaussian demands","institution":"Reliability Engineering & System Safety","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":"Crossref publication metadata. Journal: Reliability Engineering & System Safety. Authors: Peng Liu, Zude Ding, Dan Zhao, Shunguo Wang, Hao Zi. Year: 2027.","url":"https://doi.org/10.1016/j.ress.2026.113016","contact":"Peng Liu, Zude Ding, Dan Zhao, Shunguo Wang, Hao Zi","deadline":"2027","source":"Crossref","priority":6,"created_at":"2026-06-27T21:51:40.076393","quality_score":0,"quality_reason":""},{"id":356,"type":"publication","title":"A semi-analytic model of the bouncing barrier for protoplanetary dust aggregates","institution":"arXiv","country":"International","city":"","latitude":null,"longitude":null,"tags":"arxiv,publication,preprint","description":"Collisional bouncing limits the growth of dust aggregates in protoplanetary disks, but its dependence on aggregate size, collision velocity, and filling factor remains poorly understood. Here we develop a semi-analytic model for the sticking probability of colliding dust aggregates. We divide each aggregate collision into two phases: a compression phase and a separation phase. The compression phase is described with an elastoplastic contact model, which determines the maximum contact radius and repulsive energy after compression. The separation phase is treated as fracture of a stochastic network of interparticle bonds, whose fracture energy is evaluated using weakest-link statistics. The model naturally predicts that larger aggregates bounce more readily because larger contact regions are more likely to contain weak bonds. Comparison with distinct element method simulations shows that the model reproduces the simulated sticking--bouncing boundary. Furthermore, applying the calibrated model to moderately porous aggregates inferred from ALMA observations of protoplanetary disks, we find that the predicted bouncing barrier passes through the observationally inferred size--velocity ra","url":"http://arxiv.org/abs/2606.26491v1","contact":"","deadline":"2026-06-25T00:51:34Z","source":"arXiv","priority":5,"created_at":"2026-06-27T21:27:28.763349","quality_score":73,"quality_reason":"priority=5, has_url, trusted_source, good_description, detailed_description, good_tags"},{"id":1012,"type":"publication","title":"A year at EPB, 2025 Activity Report","institution":"OpenAlex","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,political science,european research area,relocation,european community,action (physics),regional science","description":"A year at EPB: 2025 Activity Report presents an overview of the activities, achievements, and strategic developments of the European Polar Board (EPB) during 2025. Marking its 30th anniversary, the report highlights a year characterised by organisational transition, strengthened coordination, and continued engagement across the European and international polar research landscape. Key developments include the relocation of the EPB Secretariat to Umeå, Sweden, and the integration of the European Polar Coordination Office (EPCO), reinforcing EPB’s role as a central platform for coordination, cooperation, and dialogue within the European polar research community. The report outlines EPB’s contributions to European policy discussions, particularly in relation to the upcoming Framework Programme 10 (FP10) and the EU Multiannual Financial Framework, as well as its engagement in EU-funded projects, international partnerships, and global initiatives such as preparations for the Fifth International Polar Year (2032–2033) and the UN Decade of Action for Cryospheric Sciences (2025–2034). It also presents highlights from EPB Members across Europe, showcasing the breadth of scientific activities, infrastructures, and collaborations that underpin European polar research. Overall, the report emphasises EPB’s continued commitment to fostering coordination, enhancing visibility, and supporting a connected, responsive, and impactful polar research community in Europe and beyond.","url":"https://doi.org/10.5281/zenodo.19436987","contact":"European Polar Board","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1470,"type":"publication","title":"ANALYSIS OF THE EFFECTIVENESS OF ISLAMIC BOARDING SCHOOL-BASED LEARNING IN IMPROVING UNDERSTANDING OF ISLAMIC TEACHINGS","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,journal article,Effectiveness, Islamic Boarding School-Based Learning, Understanding of Islamic Teachings.","description":"Journal article. This study aims to analyze the effectiveness of Islamic boarding school-based learning in improving the understanding of Islamic teachings among students (students). This qualitative research was conducted using a case study approach in one Islamic boarding school. The research sample consisted of 20 students who had participated in the Islamic boarding school-based learning program for 6 months. The results of the study indicate that Islamic boarding school-based learning is effective in improving the understanding of Islamic teachings among students. Students who participated in the Islamic boarding school-based learning program showed a significant increase in their understanding of Islamic teachings, especially in terms of understanding the principles of Islamic teachings and being able to apply Islamic teachings in their daily lives. In addition, the study also found that factors influencing the effectiveness of Islamic boarding school-based learning include the quality of the teachers, the students' motivation, and support from family and community. The conclusion of this study is that Islamic boarding school-based learning can be an effective alternative in improving the understanding of Islamic teachings among students. Therefore, the government and educational institutions need to prioritize Islamic boarding school-based learning to improve the quality of religious education in Indonesia. Python source code implementing the four-layer diagnostic framework used in the The framework comprises: Also included: scripts to regenerate publication figures (900 DPI) and Restricted raw inputs (NOT included in this archive): Derived de-identified datasets are archived separately on Zenodo (see Related Gastronomy competitions are increasingly recognised as public arenas in which culinary practices are performed, evaluated and culturally reproduced. Previous studies have mostly examined such events in relation to tourism promotion, destination visibility and economic outcomes, while their cultural role in the transmission, representation and sustainability of culinary culture has remained comparatively underexplored. Guided by the research question “Through which mechanisms do gastronomy competitions produce cultural sustainability?”, this study examines the meanings attributed to the competition experience by stakeholders involved in the Gaziantep National Cooking Competition. An interpretive qualitative research design was adopted. Semi-structured interviews were conducted with 38 stakeholders, including competitors, jury members, organisers, academics and gastronomy professionals. The data were analysed following Braun and Clarke’s thematic analysis approach. The findings show that gastronomy competitions contribute to culinary sustainability through the mechanisms of performative representation of cultural identity, experiential learning, intergenerational knowledge transfer, authenticity negotiation and selective visibility. However, competitions may also narrow the diversity of culinary heritage by prioritising recognisable and symbolic dishes. The study conceptualises gastronomy competitions as “mediating cultural infr","url":"https://doi.org/10.5281/zenodo.20966612","contact":"CAN, Meryem, MISIR, Samet","deadline":"2026-06-27","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":1235,"type":"publication","title":"Array processing in cryoseismology: a comparison to network-based approaches at an Antarctic ice stream","institution":"The Cryosphere","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":" This book \"Astronomy in Culture - Cultures of Astronomy\" provides a cultural history of astronomy. After a keynote on the efforts to protect the dark sky as an intangible global heritage admired of all cultures under the World Heritage Convention, tangible places of astronomical heritage are described. Archaeoastronomical sites from different continents and astronomical observatories from the late Middle Ages to the 21st century are presented as cultural heritage (material culture) in Chapter 2. Chapter 3 outlines some intangible astronomical heritage of Antiquity to the Middle Ages. Astronomical observations in all cultures are the basis for time keeping and calendars all over the world. Constellations are represented as figures resembling animals or seasonal activities, and seasonal climate determines rituals and cultural festivals. Chapter 4 is devoted to some astronomical heritage presented in modern planetariums and museums representing the modern culture. A highlight is the network study of patterns stored in the planetarium software \"Stellarium\". Chapter 5 contains some cross-cultural comparisons involving the whole sky. Scholars from different academic backgrounds (archaeology, history of science, philology, art history, planetarium educators, computer/data science) present their studies of this traditional knowledge and how it has been transmitted and transformed over the millennia in the seven chapters of this impressive book. Dieses Buch \"Astronomie in der","url":"https://doi.org/10.5281/zenodo.20932251","contact":"Hoffmann, Susanne M., Wolfschmidt, Gudrun","deadline":"2022-09-01","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":363,"type":"publication","title":"Automated Galerkin time stepping in Irksome","institution":"arXiv","country":"International","city":"","latitude":null,"longitude":null,"tags":"arxiv,publication,preprint","description":"As the study of temporal and spatial discretization schemes continues to advance, recent work has focused on the use of Galerkin-in-time discretization schemes that enable broader structure-preservation than is known for Runge-Kutta integrators. While the promise of such discretizations is immense, their realization has, until now, generally relied on bespoke implementations that have limited their wider use. In this work, we present automation in Irksome for both discontinuous Galerkin and continuous Petrov-Galerkin time stepping of semidiscrete variational problems. The implementation supports auxiliary variables, flexible temporal quadrature, and monolithic algebraic solvers, and it enables switching between Runge-Kutta and Galerkin-in-time formulations with minimal changes to user code. Numerical examples illustrate accuracy, solver performance, and structure preservation across representative PDE systems.","url":"http://arxiv.org/abs/2606.27300v1","contact":"","deadline":"2026-06-25T17:21:38Z","source":"arXiv","priority":5,"created_at":"2026-06-27T21:27:28.763349","quality_score":73,"quality_reason":"priority=5, has_url, trusted_source, good_description, detailed_description, good_tags"},{"id":375,"type":"publication","title":"Bayesian three-dimensional seismic travel-time tomography for active- and passive-source seismic data using physics-informed neural network","institution":"arXiv","country":"International","city":"","latitude":null,"longitude":null,"tags":"arxiv,publication,preprint","description":"Accurate 3D seismic velocity modeling through seismic travel-time tomography using both active- and passive-source data provides critical underpinning models for seismicity monitoring and hazard assessment. Because travel-time tomography is an inherently ill-posed inverse problem, UQ of the estimated models using Bayesian methods is also important for reliable downstream interpretations and analyses. However, Bayesian inference for 3D tomography based on conventional grid-based representations faces the ``curse of dimensionality'' and severe computational bottlenecks. Consequently, rigorous Bayesian UQ for margin-wide 3D travel-time tomography has remained largely unexplored. In this study, we propose a meshless 3D Bayesian travel-time tomography method that combines PINNs with a neural representation of the velocity structure, enabling tractable and data-efficient Bayesian inference through function-space particle-based variational inference. To efficiently integrate passive-source data into the Bayesian estimation of the velocity structure, we conduct analytical marginalization treating uncertain source parameters as nuisance parameters, with passive-source relocation carried out","url":"http://arxiv.org/abs/2606.21789v1","contact":"","deadline":"2026-06-19T22:40:56Z","source":"arXiv","priority":5,"created_at":"2026-06-27T21:27:28.763349","quality_score":73,"quality_reason":"priority=5, has_url, trusted_source, good_description, detailed_description, good_tags"},{"id":396,"type":"publication","title":"Belgian Array and Mobile Seismic Network","institution":"Royal Observatory of Belgium","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,seismology,geology,ambient noise level,seismic noise,aftershock,seismic array","description":"The Belgian Array and Mobile Seismic Network (BEAMS) supports Belgian scientific research in seismology. The network contains single stations or arrays that were temporarily installed either in and around Belgium, or globally in collaboration with a Belgian institution. The network includes deployments installed for seismic microzonation, single-station ambient noise mapping, rapid aftershock deployment, array deployments for site characterisation and cryoseismology, ambient noise interferometry, and shallow subsurface and geothermal research. The network is maintained by the Royal Observatory of Belgium.","url":"https://doi.org/10.7914/zgda-n457","contact":"Koen Van Noten, Thomas Lecocq, Raphaël De Plaen, Giovanni Rapagnani, & contributors","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":343,"type":"publication","title":"Beyond the equation of state: a second-order diagnostic for dynamical dark energy","institution":"arXiv","country":"International","city":"","latitude":null,"longitude":null,"tags":"arxiv,publication,preprint","description":"The first-order continuity equations determine the evolution of the energy densities but depend only on the instantaneous value of the dark-energy equation-of-state parameter. Differentiating these equations with respect to e-fold time introduces the term $ω'_{\\rm DE}$ explicitly, providing a second-order probe of dark-energy dynamics. Consequently, while information about the evolution of the equation of state is encoded in the full dynamical solution, it is not explicit in the first-order continuity equations evaluated at a given epoch. The second-order formulation, therefore, provides a complementary description in which the local evolution of the equation of state appears directly through the curvature of the density trajectory. For a two-fluid interacting dark-sector model with linear coupling $Q_{AB}=αρ_AH$, the resulting second-order equation defines a curvature diagnostic, $\\mathcal{C}=ρ_{DE}''/ρ_{DE}$, whose leading contribution, in the cosmological-constant limit, is $α^2$, while departures from $ω_{DE}=-1$ generate corrections through both $δω=1+ω_{DE}$ and the distinctive term $-3ω_{DE}'$. Unlike first-order analyses, this contribution is independent of the interaction ","url":"http://arxiv.org/abs/2606.27356v1","contact":"","deadline":"2026-06-25T17:57:16Z","source":"arXiv","priority":5,"created_at":"2026-06-27T21:27:28.763349","quality_score":73,"quality_reason":"priority=5, has_url, trusted_source, good_description, detailed_description, good_tags"},{"id":582,"type":"publication","title":"Carbonate Chemistry in Groundwater and Rivers Draining to the Baltic Sea: Implications for Coastal Ocean Acidification","institution":"University of Gothenburg, Southern Cross University","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,submarine groundwater discharge,alkalinity,groundwater,dissolved organic carbon,carbonate,seawater","description":"Abstract Terrestrial inputs can alter total alkalinity (TA) and dissolved inorganic carbon (DIC) of the coastal ocean and modify seawater pH. Here, we first characterize the carbonate system in river and groundwater draining to the Baltic Sea using observations of TA, DIC, δ 13 C-DIC, and major ions across 6 countries and 17 beaches. We then assess whether submarine groundwater discharge (SGD) may impact coastal acidification. TA and DIC concentrations were about 2 times greater in groundwater than river water. 84% of the groundwater and 72% of river samples showed potential to acidify receiving Baltic Sea waters and degas CO 2 due to low TA/DIC ratios. Mixing plots revealed non-conservative production of TA and DIC in subterranean estuaries. δ 13 C-DIC values imply that organic matter respiration was a main source of DIC to northern catchments, while calcium carbonate (CaCO 3 ) dissolution was more important along the southeastern coast. Fresh SGD contributed only < 2% of TA and DIC, and 5–7% of Ca, Mg, and SO 4 fluxes compared to river discharge when extrapolated to the entire Baltic Sea. However, unquantified total SGD (fresh groundwater plus recirculated seawater) water and chemical fluxes are likely higher. Overall, SGD can locally acidify the Baltic Sea and should be considered in regional carbon budgets.","url":"https://doi.org/10.1007/s12237-026-01761-y","contact":"Solveig Börjesson, Wilma Ljungberg, Tristan McKenzie, Gloria Reithmaier, Claudia Majtényi-Hill, Linnea Henriksson, Ceylena Holloway, Yvonne Y. Y. Yau","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1023,"type":"publication","title":"Century-Scale Earth Observation: Systematic Review of Georeferencing Methods for Historical Aerial and Satellite Imagery","institution":"University of Florida","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,georeference,remote sensing,satellite imagery,earth observation,satellite,computer science","description":"Historical remote sensing imagery, including archival aerial photographs and declassified satellite imagery, has been increasingly used to extend earth observation records into periods not covered by modern satellite missions. However, the broader application of these data remains constrained by georeferencing challenges related to incomplete metadata, uncertain acquisition geometry, and heterogeneous image characteristics. This systematic review examines georeferencing practices for historical remote sensing imagery. Out of the 2547 studies identified in the literature, 205 peer-reviewed journal articles were deemed eligible for analysis. This systematic review provides the first comprehensive, PRISMA-compliant synthesis of georeferencing practices for historical remote sensing imagery, analyzing 205 peer-reviewed studies to establish methodological patterns and identify critical gaps. The review considers imagery types, spatial and temporal distributions of case studies, georeferencing workflows, geometric constraints, and accuracy reporting practices. The results indicate a strong reliance on ground control points and a clear preference for manual or semi-automatic georeferencing approaches, while fully automatic methods remain rare. Although the use of historical imagery has increased over time, its potential has not been fully exploited due to persistent georeferencing difficulties, and study areas are often spatially limited or selectively processed to achieve acceptabl","url":"https://doi.org/10.3390/rs18071052","contact":"Wei Liu, D J Yang","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1270,"type":"publication","title":"Characterization of Pore–Fracture structures in anthracite driven by K-SVD dictionary learning and unsupervised clustering","institution":"Fuel","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":"Crossref publication metadata. Journal: Fuel. Authors: Yongxing Shen, Zengchao Feng, Dong Zhou. Year: 2027.","url":"https://doi.org/10.1016/j.fuel.2026.140039","contact":"Yongxing Shen, Zengchao Feng, Dong Zhou","deadline":"2027","source":"Crossref","priority":6,"created_at":"2026-06-27T21:51:40.076393","quality_score":0,"quality_reason":""},{"id":1246,"type":"publication","title":"Chasing the melting ice: evidence for the earliest Holocene glacier minimum in the Alps and precise dating of the subsequent advance at the end of the Preboreal","institution":"Quaternary Science Reviews","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":"Crossref publication metadata. Journal: Quaternary Science Reviews. Authors: Kurt Nicolussi, Melaine Le Roy, Irka Hajdas, Thomas Pichler, Lukas Wacker, Christian Schlüchter. Year: 2026.","url":"https://doi.org/10.1016/j.quascirev.2026.109962","contact":"Kurt Nicolussi, Melaine Le Roy, Irka Hajdas, Thomas Pichler, Lukas Wacker, Christian Schlüchter","deadline":"2026","source":"Crossref","priority":6,"created_at":"2026-06-27T21:51:40.076393","quality_score":0,"quality_reason":""},{"id":1228,"type":"publication","title":"Cirrenalia Meyers & R. T. Moore","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,taxonomic treatment,Biodiversity,Taxonomy,Fungi,Ascomycota,Sordariomycetes,Microascales,Halosphaeriaceae,Cirrenalia","description":"Taxonomic treatment. Cirrenalia Meyers & R. T. Moore, Amer. J. Bot. 47 (5): 346 (1960) Description. Saprobic on plant debris and soil in marine, freshwater and soil habitats. Sexual morph. Undetermined. Asexual morph. Conidiophores present or obsolete, cylindrical, septate or nonseptate, acrogenous or laterally on the hyphae, hyaline or light brown. Conidiogenous cells monoblastic, integrated, terminal, determinate. Conidia acrogenous, solitary, helicoid, septate, constricted or not constricted at the septa, brownish, conidial cells increase in diameter and pigmentation from base to apex. Type species. Cirrenalia macrocephala (Kohlm.) Meyers & R. T. Moore, Amer. J. Bot. 47 (5): 347 (1960). Notes. Cirrenalia species were described and recorded from marine, freshwater and terrestrial habitats on plant remains and soil. Molecular data (Fig. 4) places Cirrenalia macrocephala in the new genus Remisporiopsis with high support and therefore it has been excluded from Cirrenalia. However, other Cirrenalia species have been described including two marine species (Kohlmeyer 1958, 1968; Raghukumar et al. 1988) and 10 terrestrial species (Sutton 1973; Rao and Reddy 1978; Matsushima 1980, 1996; Sugiyama 1981; Mel’nik 1988; Somrithipol et al. 2002; Zhao and Liu 2005; Jiang and Zhang 2007; Zhang et al. 2014; Hernández-Restr","url":"https://doi.org/10.5281/zenodo.20849739","contact":"Dayarathne, Monika C., Jones, E. B. Gareth, Bahkali, Ali H., Devadatha, Bandarupalli, Hyde, Kevin D., Abdel-Wahab, Mohamed A., Calabon, Mark S., Correia, Pedro","deadline":"2026-06-25","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:44:55.032906","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1267,"type":"publication","title":"Closed-form solution of a Griffith crack in a cross-coupled hygrothermoelastic medium with moisture–thermal interaction","institution":"Applied Mathematical Modelling","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":"Crossref publication metadata. Journal: Applied Mathematical Modelling. Authors: Jine Li, Baolin Wang. Year: 2027.","url":"https://doi.org/10.1016/j.apm.2026.117145","contact":"Jine Li, Baolin Wang","deadline":"2027","source":"Crossref","priority":6,"created_at":"2026-06-27T21:51:40.076393","quality_score":0,"quality_reason":""},{"id":1054,"type":"publication","title":"Co-ordinated shifts in deep-water formation and Gulf Stream migration during abrupt climate changes","institution":"National Oceanography Centre, University College London, Royal Holloway University of London, Universität Hamburg, University of St Andrews, Woods Hole Oceanographic Institution","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,younger dryas,north atlantic deep water,gulf stream,geology,oceanography,atlantic equatorial mode","description":"Theory and models suggest the Gulf Stream may shift northwards under projected Atlantic Meridional Overturning Circulation weakening. Yet Gulf Stream behaviour during past abrupt cold events remains poorly constrained. Here we present high-resolution paleoceanographic records from the Northwest Atlantic during the last deglaciation. During the Younger Dryas cold period, we document a northward Gulf Stream shift evidenced from coherent surface and subsurface warming. Our sortable silt data suggest a strengthening of upper North Atlantic Deep Water that opposes weakening lower North Atlantic Deep Water, consistent with a seesaw feedback between the Nordic overflows and subpolar gyre. Our results constrain a co-ordinated sequence at the Younger Dryas onset: initial lower North Atlantic Deep Water weakening and subpolar sea‑ice expansion, lagged (58 ± 38 yr) by an increase in upper North Atlantic Deep Water and an eventual atmospheric reorganization (84 ± 51 yr after onset). These findings provide empirical support for model projections of future Gulf Stream shifts.","url":"https://doi.org/10.1038/s41467-026-73832-4","contact":"Fangjingcheng Zhu, Alice Carter-Champion, Jack Wharton, Joel Bracamontes‐Ramírez, Andrea Burke, Peter B. de Menocal, David Fairman, Lloyd D. Keigwin","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":965,"type":"publication","title":"Coastal Biogeochemical and Microbial Responses to Exports from a Small Rain-Dominated River Plume in the Northeast Pacific Coastal Temperate Rainforest","institution":"OpenAlex","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,biogeochemical cycle,environmental science,estuary,biogeochemistry,bay,oceanography","description":"The Northeast Pacific Coastal Temperate Rainforest (NPCTR) spans over 2000 km from Alaska to California and includes 1000's of diverse small rain-dominated coastal watersheds that, despite covering 24% of the surface area, deliver 33% of discharge to the Pacific Ocean. Coastal ecosystems receiving these inputs are potential hotspots of biogeochemical transformation but remain understudied due to logistical and historical biases of the fields of oceanography and limnology. This lack of integration across these fields limits our understanding of how terrestrial exports from small catchments affect coastal carbon and nutrient dynamics, microbial community structure, and overall ecosystem ecology. This thesis addresses this problem by examining a river-ocean estuary on Quadra Island (British Columbia, Canada) to assess how rain-dominated watershed exports shape coastal microbiology and biogeochemistry. Water samples collected within a small river plume (0-27.9 PSU) at 0, 15, and 50 cm depth across seven sites from Hyacinthe Creek into Hyacinthe Bay were analyzed for phosphate, silica, carbon and nitrogen species and isotopes, dissolved organic matter (DOM) composition, and putative active (RNA) and present (DNA) microbial communities. The core of this thesis is a manuscript that analyses carbon and nutrient concentrations, stable isotope signatures, and microbial community diversity to investigate how vertical and horizontal salinity gradients affect dispersion of organic and ino","url":"https://doi.org/10.20381/ruor-31958","contact":"R. Whalen","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1430,"type":"publication","title":"Code Smells in Clojure: Initial Findings from a Grey Literature Review","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,other","description":"Other. This contains the codes used to process SAC seismic data obtained on Argentière glacier from 2017 to 2019 and extract the associated seismic power to then investigate the subglacial hydrology properties. These codes are associated to the paper 'Quantification of seasonal and diurnal dynamics of subglacial channels using seismic observations on an Alpine Glacier' from Nanni et al., 2020 accepted in TC. La contaminación hídrica por metales pesados en un contexto de cambio climático representa un problema ambiental de fundamental importancia en la actualidad. Los ríos y aguas subterráneas están siendo afectados por vertidos domésticos, mineros e industriales que introducen elementos tóxicos como cadmio, zinc, manganeso, mercurio y plomo, los cuales se acumulan en los ecosistemas acuáticos y agrícolas. Por otro lado, el cambio climático agrava esta situación al modificar los patrones de precipitación y temperatura, generando sequías e inundaciones que facilitan la movilización y concentración de metales pesados en el agua. En zonas mineras, las lluvias intensas arrastran residuos metálicos hacia los ríos, mientras que la escasez hídrica obliga a la reutilización de aguas contaminadas en la agricultura, afectando cultivos y suelos agrícolas. El uso de estas aguas contaminadas para riego o consumo humano provoca enfermedades crónicas como daños renales, alteraciones neurológicas, cáncer y problemas en el desarrollo infantil. Además, los metales pesados no se degradan, permanecen en el ambiente y se acumulan en la cadena alimentaria, generando impactos prolongados en la salud humana y los ecosistemas. El objetivo de este estudio fue realizar un análisis bibliométrico ","url":"https://doi.org/10.61347/ei.v4i4.183","contact":"Álvarez Cabrera, Humberto","deadline":"2025-11-11","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":344,"type":"publication","title":"Continual Robot Policy Learning via Variational Neural Dynamics","institution":"arXiv","country":"International","city":"","latitude":null,"longitude":null,"tags":"arxiv,publication,preprint","description":"Robots deployed in the real world rarely operate under a single fixed dynamics model: wind changes, payloads vary, batteries drain, contacts shift, and hardware wears. Yet most learning-based controllers are trained once and deployed as if learning were complete. This prevents the robot from using deployment experience to further improve task performance. In this work, we propose a continual learning framework that uses real-world experience to improve robot policies under hidden and recurring dynamics. Our method learns a condition-aware dynamics model from real state-action trajectories by combining an analytical physics prior with a neural residual for unmodeled effects. A recurrent encoder infers the current hidden condition from recent interaction, and this estimate conditions both the residual model and the policy. Policy learning is performed via differentiable simulation using diverse learned dynamics sampled from the latent model. At deployment, these sampled conditions are replaced by conditions inferred online from recent real interaction, allowing the policy to recover recurring dynamics by recognition rather than residual re-fitting. Through extensive simulation studie","url":"http://arxiv.org/abs/2606.27353v1","contact":"","deadline":"2026-06-25T17:56:04Z","source":"arXiv","priority":5,"created_at":"2026-06-27T21:27:28.763349","quality_score":73,"quality_reason":"priority=5, has_url, trusted_source, good_description, detailed_description, good_tags"},{"id":268,"type":"publication","title":"Contrasting Climate Stressors in Permafrost Regions: Maritime Kamchatka and Continental Yakutia","institution":"Piri Reis University","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,permafrost,climate change,climatology,arctic,climate extremes,environmental science","description":"Publication from OpenAlex. Authors: Ahmet Hakan Özkan. Year: 2026","url":"https://doi.org/10.21203/rs.3.rs-9594748/v1","contact":"Ahmet Hakan Özkan","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:18:32.932503","quality_score":68,"quality_reason":"priority=6, has_url, trusted_source, good_tags, has_contact_or_authors"},{"id":1282,"type":"publication","title":"Contrasting ice nucleating particles abilities in urban and high-altitude mountain sites during the rainy season","institution":"Atmospheric Research","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":"Crossref publication metadata. Journal: Atmospheric Research. Authors: Emma Negrete-Harper, Graciela B. Raga, Rocío García, Sebastián Mendoza-Téllez, Luis A. Ladino. Year: 2026.","url":"https://doi.org/10.1016/j.atmosres.2026.109172","contact":"Emma Negrete-Harper, Graciela B. Raga, Rocío García, Sebastián Mendoza-Téllez, Luis A. Ladino","deadline":"2026","source":"Crossref","priority":6,"created_at":"2026-06-27T21:51:40.076393","quality_score":0,"quality_reason":""},{"id":1272,"type":"publication","title":"Correlating microstructural properites of ice cream made in a continuous scraped surface freezer with residence time distribution and processing parameters","institution":"Journal of Food Engineering","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":"Crossref publication metadata. Journal: Journal of Food Engineering. Authors: Lauren R. Gallagher, Richard W. Hartel. Year: 2027.","url":"https://doi.org/10.1016/j.jfoodeng.2026.113218","contact":"Lauren R. Gallagher, Richard W. Hartel","deadline":"2027","source":"Crossref","priority":6,"created_at":"2026-06-27T21:51:40.076393","quality_score":0,"quality_reason":""},{"id":1252,"type":"publication","title":"Corrigendum to “Ecological response of a glacier-fed peatland to late Holocene climate and glacier changes on subantarctic South Georgia” [Quat. Sci. Rev. 250 (2020) 106679]","institution":"Quaternary Science Reviews","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":"Crossref publication metadata. Journal: Quaternary Science Reviews. Authors: Zhengyu Xia, Lea Toska Oppedal, Nathalie Van der Putten, Jostein Bakke, Zicheng Yu. Year: 2026.","url":"https://doi.org/10.1016/j.quascirev.2026.110008","contact":"Zhengyu Xia, Lea Toska Oppedal, Nathalie Van der Putten, Jostein Bakke, Zicheng Yu","deadline":"2026","source":"Crossref","priority":6,"created_at":"2026-06-27T21:51:40.076393","quality_score":0,"quality_reason":""},{"id":865,"type":"publication","title":"Crop Water Consumption at Lake Sevan, Armenia","institution":"OpenAlex","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,evapotranspiration,water balance,environmental science,agriculture,precipitation,hydrology (agriculture)","description":"Lake Sevan, 1242 km² large, is the largest lake in the Caucasus and also Armenia. This mountain lake serves as a natural water reservoir for the Hrazdan River, which is critical for the water supply to the capital Yerevan, and the Ararat Valley, the most important agricultural region of Armenia. The annual outflow from the lake shall not exceed 170 million m³. Agriculture is an important economic sector within the lake’s basin, whereby summer and perennial crops depend on irrigation. This study used remote sensing to map the evapotranspiration of agriculture and other vegetation types to assess, in how far agriculture poses a pressure on the water balance of the lake. From 2023 to 2025, the evapotranspiration averaged across all cropland ranged between 204 mm and 307 mm, which coincides with the low yields of agriculture. During the growing season, evapo-transpiration of summer and permanent crops exceeded precipitation by 4.2 to 4.5 mil-lion m³, which is small compared to the annual outflow of 170 million m³. The annual precipitation exceeded evapotranspiration of cropland, including irrigated cropland. The findings suggest that, under current land use and climatic conditions, agriculture around Lake Sevan does not pose significant pressure on the lake’s water balance and ability to sustain its inflow into Hrazdan River.","url":"https://doi.org/10.20944/preprints202606.1456.v1","contact":"Niels Thevs, Martin Jäger, Karapet Ohanyan, Edgar Pirumyan, Varazdat Sargsyan","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":519,"type":"publication","title":"Crustal Structure and Magmatic System of Mount Erebus in Antarctica constrained by Receiver Functions and Seismic Velocity Analysis","institution":"Planetary Science Institute, Fourth Paradigm Institute, Association for the Development of Earthquake Prediction, Indian Institute of Science Education and Research Kolkata, University of the Philippines Diliman, Government Medical College","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,geology,mount,seismology,receiver function,seismic velocity,geodesy","description":"Mount Erebus, the world’s southernmost active volcano in Antarctica, offers a unique opportunity to investigate crustal controls on persistent magmatism within a caldera environment. New seismic constraints reveal a thin (~ 20 km) and compositionally heterogeneous crust beneath Erebus, consistent with long-lived lithospheric extension associated with the Terror Rift and the Ross Sea. Bulk crustal Vp/Vs ratios vary from ~ 1.61–1.94, indicating pronounced crustal heterogeneity. Elevated Vp/Vs at mid-crustal depths, combined with localized reductions in shear-wave velocity, define thermally modified zones that are consistent with intrusive complexes or transient magma storage above the Moho. While these features align with the mafic-intermediate volcanic products of Mount Erebus, interpretations invoking partial melt or compositional variations remain inherently non-unique. Additionally, a CO2 rich magma reservoir and localised silica-enriched domains could further modify crustal properties and locally reduce Vp/Vs ratio. Although deeper mantle contributions to Erebus magmatism remain unresolved, the results emphasize the importance of crustal-scale processes in sustaining long-lived volcanism beneath Mount Erebus. This study highlights the importance of integrating geophysical data to understand complex melt distribution beneath caldera systems and offers new insights into magma plumbing in extensional intraplate settings.","url":"https://doi.org/10.1038/s41598-026-48866-9","contact":"Pousali Mukherjee, Yoshihiro Ito, Kajaljyoti Borah, Emmanuel S. Garcia, Dipok K. Bora","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1405,"type":"publication","title":"Cryoseismic Signatures of Basal Ice Dynamics: Unraveling Rapid Ice Sheet Collapse Mechanisms","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,journal article","description":"Journal article. Ice sheets are critical components of the global climate system, and their dynamic response to climate change is a major source of uncertainty in sea-level rise projections. A key challenge lies in understanding the mechanisms driving rapid ice sheet collapse, which are often rooted in complex processes occurring at the ice-bed interface, known as basal ice dynamics. Traditional glaciological observations provide valuable insights but often lack the temporal and spatial resolution to capture the transient, high-frequency events associated with rapid basal changes. Cryoseismology, the study of seismic activity generated by ice, offers a unique opportunity to remotely monitor and characterize these elusive basal processes. This paper explores the potential of cryoseismic signatures to unravel the mechanisms of rapid ice sheet collapse. We review the fundamental principles of cryoseismology as applied to basal ice dynamics, detailing how various types of seismic events -- from stick-slip motion and hydraulic fracturing to subglacial sediment deformation -- can serve as indicators of specific basal processes. We propose a framework for interpreting cryoseismic data in conjunction with other glaciological observations to develop a more comprehensive understanding of the physical conditions and changes at the ice-bed interface that precede and accompany periods of accelerated ice flow. Through an in-depth analysis of hypothetical seismic event catalogs and their co","url":"https://doi.org/10.5281/zenodo.17729681","contact":"Revista, Zen, GEOGRAPHY, 10","deadline":"2025-11-27","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":227,"type":"publication","title":"Cryoseismic activity and dynamics of the Astrolabe Coastal Glacier, East Antarctica - The SEIS-ADELICE project (2020-2025)","institution":"Institut polytechnique de Grenoble, Centre National de la Recherche Scientifique, Institut National de Recherche pour l'Agriculture, l'Alimentation et l'Environnement, Université de Strasbourg, École Nationale Supérieure d'Architecture de Versailles, Institut Terre & Environnement de Strasbourg","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,astrolabe,glacier,geology,remote sensing,physical geography,data quality","description":"As part of the SEIS-ADELICE project (2020–2025), hundreds of seismological instruments were deployed on and around the Astrolabe Glacier in Terre Adélie, East Antarctica. The aim was to monitor the cryoseismic activity of an Antarctic outlet glacier as it reaches the ocean, image its internal structure and thickness, and investigate its interactions with the underlying ocean and local bedrock. This paper describes the sequential deployment of broadband, mid-band, and short-period instruments on land and at sea, the noise levels obtained in various environments and the quality of the seismological data in different frequency bands. It also presents a few non-exhaustive examples of data to demonstrate their quality and potential for analysing various cryoseismic sources at different times, frequencies, and geographic scales.","url":"https://doi.org/10.26443/seismica.v5i1.2047","contact":"Guilhem Barruol, Tifenn Le Bris, Dimitri Zigone, Florent Gimbert, Emmanuel Le Meur, Anuar Togaibekov, Denis Lombardi, Alessia Maggi","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:18:32.932503","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1237,"type":"publication","title":"Cryoseismology","institution":"Reviews of Geophysics","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":" Initial archived release of the DAS cross-correlation back-projection workflow used for the GRL manuscript. Data supporting: Interseasonal persistence of an englacial channel in a mountain valley glacier. interactive_features_all_surveys.html GPR April 2025 GPR July 2025 GPR March 2026 This educational video was produced as part of the project ALIGHT – Antarctic Living Heritage, funded by the Marie Skłodowska-Curie Actions (Horizon Europe). It introduces key issues related to the study of Antarctic cultural heritage, with particular reference to emerging cultural manifestations. Designed for educational and outreach purposes, the video aims to engage a broader audience in reflecting on the diversity and significance of cultural heritage on the continent. Production and authorship: This video was created by Gerusa Radicchi and is based on original research. The content, script, and scientific concepts were developed by Gerusa Radicchi. An artificial intelligence tool (NotebookLM) was used as a supportive resource in the video’s creation, under the author’s supervision. This educational video was produced as part of the project ALIGHT – Antarctic Living Heritage, funded by the Marie Skłodowska-Curie Actions (Horizon Europe). It introduces key issues related to documenting life and work during fieldwork in Antarctica, with particular reference to emerging cultural manifestations. Designed for educational and outreach purposes, the video aims to engage a broader audience in reflecting on the diversity and significance of cultural heritage on the continent. Production and authorship: This video was created by Gerusa Radicchi and is based on original research. The content, script, and scientific concepts were developed by Gerusa Radicchi. An artificial intelligence tool (NotebookLM) was used as a supportive resource in the video’s creation, under the author’s supervision. This study examines connections between intergroup inequality and macroeconomic Code and reproducibility package for the paper \"Energy-Efficient Hydrodynamic Flow Sensing for Autonomous Underwater Vehicles: A Spiking Neural Network Decoder for a Bio-Inspired Artificial Lateral Line with FSI Simulation and Lattice-Boltzmann CFD Validation\", submitted to Ocean Engineering. GitHub repository: https://github.com/JK-Sah/flowsnn In the Roman world, where the Mediterranean was conceptualized as Mare Nostrum, the mosaics of Antiocheia ad Orontem (hereafter Antioch) are distinguished by their rich aquatic iconography. This study focuses on the representation of freshwater fauna and flora, particularly fish, ducks, and water lilies, as seen in the mosaic from the Daphne Rasim Adalı area. In water-rich settlements such as Antioch, Daphne, and Seleucia Pieria, mosaics functioned not only as decorative programs but also as indicators of social status, wealth, and cultural identity. Aquatic creatures depicted in these mosaics draw heavily on Classical traditions, in which water is symbolically associated with life, divinity, and mythological narratives. These depictions, which include fish, ducks, and lotus or water-lily motifs, are part of a visual tradition referred to in iconography as \"Nilotic imagery\". From the Early Roman period onward, such depictions became increasingly widespread, reflecting an enduring visual vocabulary of nature and abundance. In particular, within Christian architectural contexts and elite domestic villas, representations of animals, natural landscapes, and hunting scenes were reinterpreted, acquiring new theological meanings related to purification, resurrection, and divine creation. Similar iconographic traditions can be observed in the mosaics of Antioch and its surrounding region, as well as in comparable assemblages from Zeugma and Haleplibahçe. Th","url":"https://doi.org/10.5281/zenodo.20761228","contact":"Özdilek, Banu","deadline":"2026-06-19","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":578,"type":"publication","title":"From helicopter to satellite science: shifting climate research practices in Khumbu, Nepal Himalaya","institution":"University of British Columbia, Institute for Humanities Research and Indigenous Studies of the North","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,tourism,climate change,sociology of scientific knowledge,environmental resource management,geography,citizen science","description":"Introduction The Hindu Kush Karakoram Himalaya (HKH) has been a focus of global research on the impacts of climate and cryospheric change for the past half century, yet the politics of scientific research production in this region remains underexamined. This study presents a systematic review of the climate and cryospheric research that has been conducted in the Khumbu region of the Nepal Himalaya to assess how scientific research agendas, methods and funding have evolved over the last 75 years, and to explore the ways in which the scientific community has engaged with local Sherpa communities and their knowledges. Methods Using scientometric and network analysis on the scientific literature that has been produced about the Khumbu region, we map trends in research outputs and collaboration dynamics amongst researchers and institutions, identify the major topics and foci of climate research conducted in the region, highlight shifts in methodological approaches from predominantly field-based to a focus on remote sensing, and explore how all of these factors impact engagement with local knowledges and community needs. Results We find that the scientific narratives about Khumbu and the power dynamics in knowledge production have been predominantly shaped by the interests of researchers and institutions in the Global North, particularly from researchers affiliated with academic institutions in Italy, the United Kingdom, the United States, and Japan, while local researchers are und","url":"https://doi.org/10.3389/feart.2026.1781604","contact":"Maicen Stuart, Michèle Koppes, Pasang Yangjee Sherpa","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1236,"type":"publication","title":"Frontiers in Cryoseismology","institution":"Eos","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":" This repository provides the data, code, and configuration files associated with our study titled \"Leveraging Artificial Intelligence for Predicting Human-Viral Protein-Protein Interactions: A Benchmarking Study to Address Key Challenges\". The central objective is to systematically evaluate the ability of multiple machine learning classifiers predict virus–host protein pairs, across three viral systems and under varying levels of class imbalance, conditions that closely reflect the biological reality of PPI datasets. Contents: 1. code/ — CLI pipeline for benchmarking Licensing: Code (item 1) is licensed under MIT. Negative samples and processed/derived data (items 3-4) are original work licensed under CC-BY 4.0. Positive interaction records (item 2) were sourced from public databases and remain subject to their original terms. Havispora K. L. Pang & Vrijmoed, Mycologia 100 (2): 293 (2008) Description. Saprobic on driftwood. Sexual morph. Ascomata black, ellipsoidal or subglobose, coriaceous. Periphyses absent. Peridium dark-colored, 2 - layered, outer stratum of cells ex textura angularis, inner stratum of elongated cells. Asci clavate, thin-walled, unitunicate, 8 - spored, persistent, developing at the base of ascoma venter. Catenophyses present. Ascospores ellipsoidal, thin-walled, with one appendage at each pole and four equatorial appendages of equal dimension. Appendages one tuft at polar and four tufts at equatorial positions, string-like composed of intertwining strands which split in seawater. Asexual morph. Undetermined. Type species. Havispora longyearbyenensis K. L. Pang & Vrijmoed, Mycologia 100 (2): 293 (2008). Notes. Havispora (H. longyearbyenensis) belongs to the Halosphaeriaceae with the presence of catenophyses, persistent asci with no apical structure and hyaline ascospores with appendages. Its ascospore appendage morphology and ontogeny are unique, i. e. string-like appendages composed of intertwining strands at polar and equatorial positions (Pang et al. 2008 b). Among the genera in the Halosphaeriaceae, polar and equatorial appendages are also present in the following genera: CorollosporaHavispora longyearbyenensis K. L. Pang & Vrijmoed, Mycologia 100 (2): 293 (2008) Description. Saprobic on driftwood. Sexual morph. Ascomata 442 – (616) – 787 × 306 – (422) – 607 µm, solitary, black, ellipsoidal to subglobose, immersed, coriaceous. Peridium 29 – (37) – 44 µm, dark-colored, 2 - layered, outer stratum with 5–7 rows of cells of textura angularis, inner stratum with 3–4 rows of elongated cells. Necks 43 – (61) – 80 × 33 – (69) – 88 µm, periphyses absent. Asci 88 – (103) – 114 × 20 – (25) – 33 µm, clavate, pedunculate, thin-walled, unitunicate, 8 - spored, persistent, developing at the base of the ascoma venter. Catenophyses present, 105 – (132) – 165 × 5 – (6) – 8 µm. Ascospores 24 – (30) – 36 × 8 – (11) – 14 µm, ellipsoidal, hyaline, thin-walled, 3 - septate constricted at the septa, with tufts of appendages. Appendages 4 – (10) – 14 µm long, at one polar tuft, and four tufts in an equatorial position, string-like composed of intertwining strands that split in seawater. Asexual morph. Undetermined. Notes. Havispora longyearbyenensis is saprobic on driftwood (Pang et al. 2008 b). Dist","url":"https://doi.org/10.5281/zenodo.20849805","contact":"Dayarathne, Monika C., Jones, E. B. Gareth, Bahkali, Ali H., Devadatha, Bandarupalli, Hyde, Kevin D., Abdel-Wahab, Mohamed A., Calabon, Mark S., Correia, Pedro","deadline":"2026-06-25","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":476,"type":"publication","title":"High Spatial and temporal 3D Sea Ice Thickness Reconstruction Using Seismic Waveform Inversion and Tomography","institution":"Institut des Sciences de la Terre, Université Grenoble Alpes, ESPCI Paris","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,geology,sea ice,inversion (geology),sea ice thickness,sea ice concentration,tomography","description":"Abstract. Sea ice is a porous, two-phase material whose evolution influences climate, ecosystems, and human activities in polar regions. Rapid declines in Arctic sea ice thickness highlight the need for monitoring approaches that resolve small-scale spatial variability, beyond the coarse resolution of satellite-derived products. Seismic methods, based on the analysis of seismic waves guided in the ice layer, provide high-resolution local estimates of ice thickness, but have so far been limited to individual source–receiver paths. Here, we present a methodology to generate maps of sea ice thickness from seismic data. We analyze two complementary datasets acquired on fast ice: controlled-source data recorded by a 16-geophone array in the St. Lawrence Estuary (Canada), and passive data collected by a dense 247-geophone array in Svalbard (Norway). Ice thickness is first estimated along individual paths through waveform inversion based on spectral element modeling. These path-specific estimates are then integrated within a tomographic framework to reconstruct spatially continuous sea ice thickness maps. Our results demonstrate that both active and passive seismic measurements can resolve spatial heterogeneity in ice thickness at high resolution. This seismic-tomographic approach provides a practical and scalable tool for fine-scale monitoring of sea ice in rapidly changing polar environments.","url":"https://doi.org/10.5194/egusphere-2026-2519","contact":"Hooshmand Zandi, L Métivier, Romain Brossier, Sébastien Kuchly, Vasco ZANCHI, Nicolas Mokus, Véronique Dansereau, Antonin Eddi","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":837,"type":"publication","title":"Hindu Kush-Karakoram-Himalaya Under Threat: Climate Change,Cryosphere Hazards, and the Imperative for Regional Cooperation","institution":"OpenAlex","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,cryosphere,glacial period,glacier,permafrost,climate change,environmental resource management","description":"The Hindu Kush-Karakoram-Himalaya (HKH) often described as the Third Pole because it contains the largest concentration of snow and ice outside the Arctic and Antarctic anchors Asia’s hydrological security by feeding ten major river systems and sustaining livelihoods across some of the world’s most densely populated downstream plains. The region is undergoing rapid, elevation-amplified warming and accelerating cryosphere change, including glacier mass loss, permafrost degradation, and the growth and reorganization of glacial lakes. One of the most acute manifestations of this transformation is the rising systemic risk from glacial lake outburst floods (GLOFs), low-probability but high-impact events capable of cascading across borders through shared river basins, infrastructure corridors, and coupled energy-trade systems. Drawing on the contemporary scientific literature on High Mountain Asia (HMA) cryosphere dynamics and GLOF processes, and anchoring the analysis in recent transboundary and near-transboundary flood events, this study argues that regional cooperation implemented through interoperable monitoring, real-time hydrometeorological and cryosphere data exchange, harmonized risk standards, and joint early-warning and response protocols offers a rare set of non-zero-sum gains. It can reduce disaster losses and uncertainty for the region while creating durable channels of technical trust. Building on existing regional platforms such as ICIMOD, emerging WMO Third Pole cli","url":"https://openalex.org/W7154551894","contact":"D. Erokhin","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":256,"type":"publication","title":"Historical tectonic activity along the eastern segment of the Bassano-Valdobbiadene Thrust: new hints for the seismic hazard assessment of the Venetian Prealps between Vittorio Veneto and Valdobbiadene (eastern Southern Alps, NE Italy)","institution":"University of Udine, Istituto di Ricerche Chimiche e Biochimiche G. Ronzoni","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,geology,seismology,tectonics,induced seismicity,seismotectonics,fault (geology)","description":"Abstract. In the framework of the Italian Seismic Microzonation Project, we investigated the easternmost segment of the Bassano–Valdobbiadene Thrust Auct. (i.e. the Vittorio Veneto–Valdobbiadene Thrust) which runs at the base of the Venetian prealpine foothill between Miane, Follina and Cison di Valmarino municipalities (NE Italy). The Bassano–Valdobbiadene Thrust belongs to the SW–NE striking, SE–verging Pliocene–Quaternary front of the eastern Southern Alps which at present, accommodates deformation with velocities of the order of 2–3 mm/yr. Prominent geological and morphological expression (Mt. Grappa–Mt. Cesen–Mt. Visentin anticlines) underlies the Miocene to Present tectonic activity of the Bassano–Valdobbiadene Thrust, however the Quaternary tectonic activity is scarcely constrained. The historical seismicity reveals that few destructive earthquakes (M≥5.5) hit the Venetian prealpine region, but no significant seismic events affected Follina and the surrounding areas during the last millennium. In order to investigate the recent tectonic activity of this sector of the eastern Southalpine front, we made a morphotectonic survey along the San Pietro and Soligo valleys (i.e. the Vallata valley) and, in correspondence of possible morphotectonic evidence, a series of Electroresistivity Tomography investigations. Following, we dug some paleoseismological trenches across the possible surficial trace of the tectonic structure. The results of our study pinpointed that the Vittori","url":"https://doi.org/10.5194/egusphere-2026-2658","contact":"Maria Eliana Poli, Giulia Patricelli, Giovanni Paiero, Andrea Marchesini, Enrico Farinatti","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:18:32.932503","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":747,"type":"publication","title":"Holocene evolution of permafrost-dominated nearshore environment and carbon source variability in Tuktoyaktuk Harbor, Canadian Beaufort Sea","institution":"OpenAlex","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,holocene,thermokarst,oceanography,marine transgression,permafrost,geology","description":"The Canadian Beaufort Sea is characterized by predominantly permafrost coastlines that are particularly vulnerable to coastal erosion due to high amounts of unconsolidated sediments. Additionally, the Mackenzie River transports suspended sediments and discharges large amounts of remobilized carbon nearshore. The rate at which marginal coasts erode and sediment accumulates is expected to increase with rising sea level and enhanced fluvial sediment transport. To understand how these coastal systems develop over time it is essential to investigate their past evolution. Here, a 9m long sediment core from Tuktoyaktuk Harbor was investigated to resolve past variability in sediment and terrestrial carbon delivery to the nearshore environment. The core is constrained by an age model spanning the last 10,000 years. Our results show that the site initially hosted a freshwater fen in the Early Holocene before transitioning into a thermokarst lake during the mid-Holocene. Initial marine inundation occurred at 4315±514 cal yr BP. Continued transgression transformed the site into a lagoon with strongly anoxic bottom waters. Reduced anoxia over time led to the establishment of a brackish lagoon. Over the last millennium deposits exhibit a notable increase in petrogenic carbon delivery, indicating enhanced erosion of ancient carbon stocks within the Mackenzie River watershed.","url":"https://openalex.org/W7165073163","contact":"Blanda Matzenbacher, Tommaso Tesi, Petra Zahajská, Michael Fritz, Lisa Bröder, Malin Kylander, Katharina Schwarzkopf, Julie Lattaud","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1148,"type":"publication","title":"Hotspots of Arctic and sub-Arctic marine sediment organic carbon are dominated by the Baltic, Barents and Chukchi Seas","institution":"University of Glasgow, Umeå University, Grønlands Naturinstitut","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,environmental science,total organic carbon,oceanography,arctic,carbon cycle,sediment","description":"The Arctic and sub-Arctic are warming at least three times faster than the global average, altering terrestrial carbon delivery to the oceans and marine carbon cycling. The sequestration of such carbon into marine sediments is a key contributor to climate regulation. Despite this, the location of organic carbon hotspots at high latitudes are poorly understood, hindering our ability to identify their sensitivity to environmental change. Using quantile regression forests with >13,000 sediment samples, we identify the Baltic, Barents and Chukchi Seas as the dominant high-latitude marine organic carbon hotspots, playing a disproportionately large role in the area-normalised global sedimentary carbon stock. Organic carbon accumulation rates are elevated across shallow shelf environments and coastlines, particularly in proximity to Arctic rivers. Development of organic carbon hotspots reflects both local and external processes, including salinity, mixed layer depth, primary production and sedimentation, demonstrating the importance of coupled land-ocean processes. Uncertainty in future changes to organic carbon cycling and transit pathways, including river transport, is therefore an emerging risk factor for the stability of marine sediment carbon stores. Compounding this, only 10.19% of the surface sediment organic carbon stock is currently within marine protected areas, placing >17 Pg at higher risk of anthropogenic disturbance.","url":"https://doi.org/10.1038/s43247-026-03720-8","contact":"Beth Langley, Heidi L. Burdett, Karen A. Cameron, Thomas Juul‐Pedersen, Alexandra Rouillard, Charlotte Slaymark, Nicholas A. Kamenos","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":846,"type":"publication","title":"Human Remains: Everest and the Ontological Afterlives of George Mallory and Andrew Irvine","institution":"OpenAlex","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,subject (documents),liminality,environmental ethics,philosophy,anthropocene,state of exception","description":"The philosopher Giorgio Agamben has argued that the ‘human/nonhuman distinction is the conceptual ground for any further ontological elaboration’, (Grieve-Carlson, 179) that humans must distinguish themselves from their environment and other beings before the work of culture can begin. However, objects frequently ‘problematize the boundaries of the human’ (Knutson, 273), never more so than when we encounter human remains in the process of transition from human subject to physical object. The philosopher Daniel Heller-Roazen notes ‘that a corpse is no human being seems obvious, yet it is equally certain that it is no ordinary thing…A human cadaver is neither a person nor not a person. It is a nonperson in a special sense, which requires commentary and elucidation’ (Heller-Roazen,159). On Everest, the ambiguity of post-mortal personhood is exacerbated by the preservation of human remains in liminal states in the mountain cryosphere. Human remains on Everest enter new ontic states and new spatio-temporal regimes that render these corpses uncanny. They are encountered within the mountain cryosphere as both fixed features in a landscape and as mobile entities in glacial systems. Extreme environments at altitude reduce human agency and disrupt the normal cultural approaches to disposing of human remains. The persistence of these corpses in the cryosphere and their post-mortal (im)mobilities raises important questions about the ways in which fixity and prolongation of bodies in the cr","url":"https://openalex.org/W7130241212","contact":"Jonathan Westaway","deadline":"2028","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":336,"type":"publication","title":"Hybrid NARX-LLM for Greenland Iceberg Discharge: Prompt-Driven Residual Correction","institution":"arXiv","country":"International","city":"","latitude":null,"longitude":null,"tags":"arxiv,publication,preprint","description":"Greenland iceberg discharge exhibits complex nonlinear dynamics with limited observability, challenging traditional predictive models. We present a Hybrid NARX-LLM framework that combines a nonlinear autoregressive model with exogenous inputs (NARX) and a large language model (LLM) for residual correction. We further propose a Physics-Informed Prompt (PIP) method that transforms unstructured physical knowledge into structured prompts for zero-shot in-context reasoning. The primary objective is to explore the corrective potential of this framework for modeling Greenland iceberg discharge, rather than merely optimizing predictive accuracy. The NARX component captures intrinsic temporal dependencies, while the LLM, guided by PIP, encodes glacier dynamics and environmental drivers and perceives key trend patterns to correct systematic prediction errors. This integration allows the model to reason about unmodeled factors and produce interpretable residuals, enhancing overall predictive accuracy. Applied to Greenland iceberg discharge time series, our approach addresses extreme events that are difficult to predict due to rare variations and nonstationary trends, a limitation often overlo","url":"http://arxiv.org/abs/2606.15288v1","contact":"","deadline":"2026-06-13T13:03:17Z","source":"arXiv","priority":5,"created_at":"2026-06-27T21:27:28.763349","quality_score":73,"quality_reason":"priority=5, has_url, trusted_source, good_description, detailed_description, good_tags"},{"id":359,"type":"publication","title":"Hybrid privacy-aware semantic search: SVD-truncated document geometry and CKKS-encrypted query reranking under a restricted threat model","institution":"arXiv","country":"International","city":"","latitude":null,"longitude":null,"tags":"arxiv,publication,preprint","description":"Dense embeddings power semantic search and retrieval-augmented generation, but embedding-inversion attacks can reconstruct source text from a vector: when a vector database leaks, the documents behind it leak too. The textbook defences are extremes - encrypting the whole search homomorphically is sound but too slow at million-document scale, while privacy noise degrades ranking long before it protects. We study a middle path exploiting the asymmetry between the static collection and the dynamic query. The collection is protected geometrically: each vector is truncated onto a lower-dimensional SVD subspace and rotated by a secret orthogonal transform known only to the owner. The query is protected cryptographically: it is reranked under CKKS homomorphic encryption, so an honest-but-curious server never sees the query or the scores. CKKS parameters come from a small offline benchmark. We prove a tight lower bound on the reconstruction error of any attacker confined to the protected subspace. On one million documents and five encoders the scheme preserves ranking quality (slightly improving it on strong encoders, as a linear denoiser) at sub-second latency, and an off-the-shelf invers","url":"http://arxiv.org/abs/2606.26373v1","contact":"","deadline":"2026-06-24T20:50:58Z","source":"arXiv","priority":5,"created_at":"2026-06-27T21:27:28.763349","quality_score":73,"quality_reason":"priority=5, has_url, trusted_source, good_description, detailed_description, good_tags"},{"id":1248,"type":"publication","title":"Hydrological response to glacier peak water in the largest inland river basin of China","institution":"Journal of Hydrology","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":"Crossref publication metadata. Journal: Journal of Hydrology. Authors: Haodong Lyu, Gonghuan Fang, Yaning Chen, Wenting Liang, Lei Wang, Jianmin Qiao, Man Chen, Xiaolong Yan. Year: 2026.","url":"https://doi.org/10.1016/j.jhydrol.2026.135695","contact":"Haodong Lyu, Gonghuan Fang, Yaning Chen, Wenting Liang, Lei Wang, Jianmin Qiao, Man Chen, Xiaolong Yan","deadline":"2026","source":"Crossref","priority":6,"created_at":"2026-06-27T21:51:40.076393","quality_score":0,"quality_reason":""},{"id":608,"type":"publication","title":"Hydrological variability and water stress dynamics under changing conditions: a case study of the Shu River","institution":"Ministry of Water Resources and Irrigation, Kazakh Scientific Research Veterinary Institute, Kazakh National Medical University, Yugra State University, SMART Reading","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,environmental science,hydrology (agriculture),inflow,water balance,water resources,drainage basin","description":"This study investigates hydrological variability and water stress dynamics in the Shu River basin, a semi-arid transboundary river system in Central Asia, under changing climatic and anthropogenic conditions. Using hydrological data from 2011 to 2024 collected at three key gauging stations (Kainar, Tashutkul, and Ulanbel), we analyzed temporal variations in river inflow, water balance components, and water stress indicators. A combination of statistical methods, including linear trend analysis, the Mann–Kendall test, Sen’s slope estimator, and the coefficient of variation, was applied to assess the direction, magnitude, and variability of hydrological changes. In addition, the Water Stress Index (WSI) and Environmental Flow Ratio (EFR) were used to evaluate pressure on water resources and ecological sustainability. The results reveal a consistent decline in river discharge across all observation sites, with the most pronounced decrease observed in downstream sections. Total inflow and river inflow show statistically significant negative trends, indicating a reduction in water availability over time. In contrast, local flow and water consumption exhibit no significant trends, suggesting relatively stable demand conditions. The WSI analysis indicates moderate to high water stress, with increasing variability and periodic exceedance of critical thresholds in recent years. Despite growing pressure on water resources, the EFR remains above ecological safety thresholds, indicating ","url":"https://doi.org/10.3389/fenvs.2026.1833871","contact":"Nurlan Bakbergenov, Talgat Imanaliyev, Mirobit Mirdadayev, Raikhan Beisenova","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1241,"type":"publication","title":"Ice-flux divergence and strain rates reveal compressive-flow hotspots on Gangotri glacier","institution":"Physics and Chemistry of the Earth, Parts A/B/C","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":"Crossref publication metadata. Journal: Physics and Chemistry of the Earth, Parts A/B/C. Authors: Anikul Islam, Divyesh Varade, Lavkush Kumar Patel, Aliva Nanda, Somil Swarnkar, Rajiv Sinha. Year: 2026.","url":"https://doi.org/10.1016/j.pce.2026.104482","contact":"Anikul Islam, Divyesh Varade, Lavkush Kumar Patel, Aliva Nanda, Somil Swarnkar, Rajiv Sinha","deadline":"2026","source":"Crossref","priority":6,"created_at":"2026-06-27T21:51:40.076393","quality_score":0,"quality_reason":""},{"id":1478,"type":"publication","title":"Ice-nucleating particles at Ny-Ålesund: a study of condensation freezing by the Dynamic Filter Processing Chamber","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,publication","description":"Publication. This study presents atmospheric ice-nucleating particle (INP) data from the Gruvebadet (GVB) observatory in Ny-Ålesund (Svalbard). Aerosol particle sampling activities were conducted over 3 years (2018–2020) for a total of six intensive campaigns, covering three seasons (spring, summer, and autumn), by deploying PM1 and PM10 sampling inlets in parallel. Ambient INP concentrations (nINP) were measured offline on the collected filters in condensation-freezing mode (water saturation ratio of 1.02) by means of the Dynamic Filter Processing Chamber. Three activation temperatures (T) were considered: −15, −18, and −22 °C. Overall, in the PM10 size range, nINP ranged from 0.3 to 315 m−3 in the considered T range, in agreement with previous observations in the Arctic environment. Regarding the ice nucleation efficiency of the investigated aerosol particles (referring to the range between 0.1 ","url":"https://doi.org/10.5281/zenodo.20825362","contact":"rinaldi, matteo, Nicosia, Alessia, Paglione, Marco, Mansour, Karam, Decesari, Stefano, Mazzola, Mauro, Santachiara, Gianni, Belosi, Franco","deadline":"2026-06-24","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":672,"type":"publication","title":"Ice‐Sheet–Ocean Interactions and the Reversibility of a Regime Shift Beneath Filchner‐Ronne Ice Shelf","institution":"Northumbria University, British Antarctic Survey","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,ice sheet,geology,climatology,sea ice,lead (geology),atmospheric sciences","description":"Abstract Future atmospheric warming could cause an abrupt increase in ocean temperature beneath the Filchner–Ronne Ice Shelf, Antarctica, from −2.2°C to more than 0°C in a few decades. In simulations, such a transition leads to a twenty‐fold increase in sub‐shelf melt rates, driving a retreat of the ice sheet. Here we investigate the evolution and reversibility of the ocean and ice sheet states using coupled ice‐sheet–ocean model simulations. We show that sub‐shelf melt rates increase only half as much as in the uncoupled system, and we find that, after a period of climate cooling, the cavity is reversible from warm to cold conditions, independently of ice‐ocean interactions related to regional changes in sub‐shelf melting, cavity geometry, and ocean dynamics. In contrast to the abrupt warming transition, the recovery of a cold ocean state takes more than a century. Meanwhile the ice sheet continues to lose mass and contribute to sea level rise with a maximum rate of up to 0.9 mm/a.","url":"https://doi.org/10.1029/2025jc023952","contact":"Ronja Reese, Jan De Rydt, Kaitlin A. Naughten","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":732,"type":"publication","title":"Imaging the North Bishop Block with Ambient Noise and Converted Phases Observed through Fiber-Optic Seismology","institution":"California Institute of Technology","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,geology,ambient noise level,seismology,structural basin,block (permutation group theory),rift","description":"Located in eastern California, Owens Valley is a rift basin in the western Basin and Range Province, bounded by the Sierra Nevada and White Mountains. While the basin has been the site of extensive geologic study, most interpretations of the subsurface structure depend on non-unique interpretation of gravity data. Under these constraints, past researchers have inferred the presence of the North Bishop Block, a block slumped from the White Mountains, roughly 100 square kilometers in area. A section of optical fiber near the town of Bishop, CA, in Owens Valley has been converted to a seismic array, and records apparent Ps converted phases above the proposed location of the North Bishop Block. We assume that the Ps phase is produced by the slumped block and jointly invert for a velocity structure through ambient noise cross-correlation and from the observed Ps phases, advancing the use of converted phases in fiber-optic seismic data. We replicate the proposed depth of the North Bishop Block and observe a deeper phase-converting interface to the south. We interpret this interface as an unmapped slumped block, located at roughly 1 kilometer depth. This result has important implications for the tectonic history and subsurface hydrology of Bishop, CA.","url":"https://doi.org/10.26443/seismica.v5i1.1175","contact":"Eli Bird, James Atterholt, Ettore Biondi, Yan Yang, Zhongwen Zhan","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":314,"type":"publication","title":"Impact of surface loading on stress and seismicity modulation in global subduction zones","institution":"Chalmers University of Technology","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,subduction,geology,seismology,induced seismicity,stress (linguistics),intraplate earthquake","description":"Surface mass redistribution from hydrological, atmospheric, and oceanic processes continually deforms the solid Earth and produces stress perturbations that are small in amplitude but coherent in space and periodic in time. This thesis examines whether such loading-induced stress variations are mechanically relevant for earthquake occurrence in subduction zones, and evaluates them in a tectonic context. The regional study of the Kuril Islands-Japan region resolves loading-induced stress changes onto the megathrust geometry to compute monthly Coulomb failure stress changes from hydrological, atmospheric, and non-tidal ocean loading. A weak but statistically significant correlation is found between multi-loading-induced Coulomb stress variations and seismicity in some areas, with the clearest signal in the shallow southern Kuril segment near Hokkaido. The global study uses satellite gravimetry data from the GRACE and GRACE-FO missions to compute monthly loading-induced stress variations in the upper 50 km, and projects them onto principal tectonic stress directions inferred from earthquake focal mechanisms. The projected stress perturbations are then compared with background seismicity. Results reveal faulting- and region-dependent patterns of stress modulation and seismic response across global subduction zones. Together, the results indicate that modest, periodic stress variations from surface loading can measurably modulate earthquake occurrence in parts of the subduction sy","url":"https://doi.org/10.63959/chalmers.dt/5870","contact":"Yiting Cai","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:18:32.932503","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":819,"type":"publication","title":"Implications of glacier detachment triggered by a surge event at Dehdal Glacier in the Pamir Mountains, using daily PlanetScope imagery","institution":"Chinese Academy of Sciences, Xinjiang Institute of Ecology and Geography, University of Fribourg, University of Zurich, Swiss Federal Institute for Forest, Snow and Landscape Research, University of Chinese Academy of Sciences, Academy of Sciences of the Republic of Tajikistan, Environmental Protect","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,surge,glacier,geology,tidewater glacier cycle,glacier mass balance,glacier morphology","description":"Abstract. Surge-type behavior and low-angle glacier detachments in small debris-covered mountain glaciers remain insufficiently documented. This study investigates the surge of the Dehdal Glacier in the northwestern Pamirs during 2025–2026, using daily PlanetScope satellite imagery. Multi-epoch uncrewed aerial vehicle (UAV) orthomosaics and digital elevation model (DEM) differencing from 2019 to 2023 reveal significant pre-surge internal mass redistribution, evidenced by surface thickening of the central tongue and surface lowering in both the upper glacier and the distal tongue, suggesting progressive internal destabilization. Demonstrated by PlanetScope imagery, the surge evolved through three distinct phases, which shows that surge initiation occurred internally and subsequently propagated down-glacier toward the terminus, resulting in detachments, accelerated ice flow, and reoccupation of the valley floor. Two low-angle detachments moved ice up to 4.7 km down-valley, depositing an estimated 4–5 × 106 m³ of ice on the valley floor. By January 12, 2026, the glacier had largely stabilized, with the primary glacier tongue covering approximately 1.83 km² and a detached ice mass of about 0.26 km² persisting farther downstream, resulting in a total ice area of roughly 2.09 km². Notably, the recurrence interval of 9–10 years since the previous surge is significantly shorter than the earlier 20–30-year intervals. This shortened interval is unlikely to be due to seismic activity or","url":"https://doi.org/10.5194/egusphere-2026-1923","contact":"Mustafo Safarov, Junli Li, Evan Miles, Majid Gulayozov, R K Li, Ali Fazylov, Kamoliddin Nazirzoda, Firdavs Vosidov","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1063,"type":"publication","title":"Improving global and regional ocean heat content by consistently combining GRACE gravity, satellite altimetry and Argo profile observations in a joint inversion framework","institution":"University of Bonn, University of Twente, Universität Hamburg","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,argo,ocean heat content,climatology,altimeter,inversion (geology),satellite altimetry","description":"Abstract. The current energy imbalance at the top of atmosphere and corresponding heating of the Earth system is the main driver of steric sea level change through ocean heat uptake (OHU). A global constant heat capacity factor is commonly applied to retrieve ocean heat content (OHC) from observed ocean-average steric sea level. We propose an extension to this methodology, which focuses on the leading modes of steric variability, which are derived from an ocean model and fitted to GRACE gravity, satellite altimetry and in situ Argo observations within a joint inversion framework. These modes are utilized to obtain data driven OHC estimates by establishing a mapping between modeled OHC and steric sea level, and rescaling each mode individually based on observed steric sea level change. On global scales for the period 2005-01 till 2024-12, our OHU results (0.62 W/m2) agree well with a variety of published datasets from in situ Argo data, model reanalyses and space-geodetic approaches as well as independent estimates from the CERES project. At basin scales, we demonstrate the global OHU to be driven mainly by warming of the Pacific Ocean (0.23 W/m2), followed by contributions from the Indian (0.20 W/m2) and Atlantic (0.13 W/m2) oceans. Minor contributions are found from the Arctic Ocean (0.01 W/m2), the Southern Ocean (0.02 W/m2) and the residual ocean (0.03 W/m2). Our results also indicate a shift from dominant heating in the Indian Ocean driven by heat transport from the Pacif","url":"https://doi.org/10.5194/essd-2026-368","contact":"Bernd Uebbing, Kristin Vielberg, Roelof Rietbroek, Bene Aschenneller, Armin Köhl, Jürgen Kusche","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":316,"type":"publication","title":"In Science Journals","institution":"OpenAlex","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,library science,data science,political science,computer science,medline,engineering ethics","description":"Highlights from the Science family of journals","url":"https://doi.org/10.1126/science.aei7753","contact":"Sacha Vignieri, Angela Hessler, Phil Szuromi, Madeleine Seale, Marc S. Lavine, Yury Suleymanov, Christiana N. Fogg, Leslie Ferrarelli","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:18:32.932503","quality_score":68,"quality_reason":"priority=6, has_url, trusted_source, good_tags, has_contact_or_authors"},{"id":1291,"type":"publication","title":"Incremental dynamic analysis via hierarchical Bayesian modelling for efficient seismic fragility analysis and uncertainty quantification","institution":"Reliability Engineering & System Safety","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":"Crossref publication metadata. Journal: Reliability Engineering & System Safety. Authors: Zhihui Wang, Jiangxu Deng, Jinghua Zhang, Chaozhe Zhang, Roberto Cudmani, Yong Yuan. Year: 2026.","url":"https://doi.org/10.1016/j.ress.2026.112877","contact":"Zhihui Wang, Jiangxu Deng, Jinghua Zhang, Chaozhe Zhang, Roberto Cudmani, Yong Yuan","deadline":"2026","source":"Crossref","priority":6,"created_at":"2026-06-27T21:51:40.076393","quality_score":0,"quality_reason":""},{"id":1429,"type":"publication","title":"Instructor–learner interactions in EFL speaking contexts: A qualitative thematic analysis","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,journal article,lnstructor leaner interaction","description":"Journal article. I This article investigates how English as a Foreign Language (EFL) students perceive instructor–learner interaction in academic speaking classrooms. Using a qualitative thematic analysis of responses from 39 university students, the study explores the interpersonal and pedagogical factors that encourage or discourage oral participation. The findings identify three major themes: (1) affective safety as a prerequisite for speaking, where supportive instructor behaviors and positive nonverbal communication reduce learners' anxiety; (2) a preference for indirect, meaning-focused corrective feedback, which allows students to maintain communicative flow while developing language accuracy; and (3) the need for equitable and invitational classroom interaction, emphasizing fair turn-taking, appropriate wait time, and inclusive participation opportunities. The study concludes that effective instructor–learner interaction extends beyond linguistic instruction by fostering emotional support, learner confidence, and equitable participation. It argues t","url":"https://doi.org/10.5281/zenodo.20957750","contact":"POURFEIZ, Jafar","deadline":"2026-06-26","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":1230,"type":"publication","title":"Integrative description of two new tardigrade species from the rainforests of Kibale National Park, Uganda","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,journal article,Africa,DNA barcoding,Haplotype network,Taxonomy,Water bears","description":"Journal article. Abstract African tropical forests are highly underexplored regarding microinvertebrate diversity, including tardigrades. Here, we describe two new tardigrade species from the genera Parahypsibius Gąsiorek et al., 2024 and Echiniscus C.A.S. Schultze, 1840, collected in the tropical rainforest of the Kibale National Park in southwestern Uganda. Species delimitation was based on an integrative approach combining morphological, morphometric, and molecular data. Morphological analyses employed light and scanning electron microscopy, while molecular characterization used mitochondrial COI and nuclear 18S rRNA, 28S rRNA, ITS1, and ITS2 markers. Additionally, we report Echiniscus lineatus Pilato, Fontoura, Lisi and Beasley, 2008 from Uganda for the first time, providing new sequences and reconstructing haplotype networks using previously published genetic data of this species. Phylogenetic analyses of subfamily Hypsibiinae Pilato, 1969 and genus Echiniscus clarify the relationships of the new taxa and place them within the broader phylogenetic context. Our study highlights the underestimated diversity of African tardigrades and demonstrates the importance of integrative taxonomy for species delineation. The new records from Kibale National Park provide also baseline data for understanding the distribution and phylogeny of tardigrades of the Central Africa. Scripts for producing the results in submitted paper: Variable ice-rock coupling near the grounding zone of Totten Glacier, East Antarctica, inferred from repeating stick-slip icequakes. Nona Dronova, Dr.Sc. (Tech.) Chairperson, Expert Collegium on Antiques | Certified Gemmologist (40 years' practice) Submitted: June 2026 | Licence: CC BY 4.0 Three circular seal paste boxes (yínse hé, 印色盒) attributed to the Kangxi reign period of the Qing dynasty (1662–1722) were examined using optical gemmological microscopy combined with visual pigment analysis and epigraphy. Object KX-DSB-B&W-01 is a blue-and-white porcelain box bearing a four-character hall mark 安素草堂制 (Ānsù Cǎotáng zhì, \"Made for the Studio of Simple Elegance\"). Object KX-DSB-DC-02 is a doucai (斗彩) polychrome box with a lotus-and-carp (yúzǎo, 鱼藻) design and a six-character reign mark 大清康熙年製 within a double circle. Object KX-DSB-DC-03 is a second doucai box decorated with an auspicious peach-and-bat (shòutáo, 寿桃) motif, also carrying the six-character Kangxi mark. Microscopic assessment of glaze depth, cobalt underglaze tonality,","url":"https://doi.org/10.5281/zenodo.20935539","contact":"Дронова, Нона","deadline":"2026-06-26","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":376,"type":"publication","title":"Optimization and robustness of cost-efficient seismic arrays for Newtonian noise cancellation at the Einstein Telescope","institution":"arXiv","country":"International","city":"","latitude":null,"longitude":null,"tags":"arxiv,publication,preprint","description":"Newtonian noise is expected to be the dominating noise source for low frequencies at the Einstein Telescope. It originates from seismic waves that cause density fluctuations in the rock around the interferometer. The mitigation strategy for Newtonian noise relies on an array of seismometers, placed at depth in boreholes, which provides measurements of the seismic wave field. We optimize the positions of the individual seismometers for the mitigation capabilities of the array for a full corner of the Einstein Telescope. We find that the mitigation capabilities of arrays with multiple seismometers in each borehole match the capabilities of only somewhat smaller arrays but with only one seismometer per borehole. Mitigation is further improved by extending the array with seismometers in the interferometer tunnels. Such configurations may hence provide a cost-effective way towards realizing an efficient seismic array. In each case, we quantify the broadband mitigation performance in the range from 1 to 10 Hz for arrays that are optimized for a frequency of 10 Hz, as well as the robustness of the arrays with respect to variations from their optimized positions. We find that larger arrays","url":"http://arxiv.org/abs/2606.21110v1","contact":"","deadline":"2026-06-19T05:28:45Z","source":"arXiv","priority":5,"created_at":"2026-06-27T21:27:28.763349","quality_score":73,"quality_reason":"priority=5, has_url, trusted_source, good_description, detailed_description, good_tags"},{"id":1279,"type":"publication","title":"Optimization of extrusion process in enhancing shelf stability and bioactive compounds of black rice bran","institution":"Future Foods","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":"Crossref publication metadata. Journal: Future Foods. Authors: Dong Zhao, Qi Tan, Mingwei Zhang, Donghwa Chung, Xuchao Jia, Xing Meng, Fei Huang, Lihong Dong. Year: 2026.","url":"https://doi.org/10.1016/j.fufo.2026.101061","contact":"Dong Zhao, Qi Tan, Mingwei Zhang, Donghwa Chung, Xuchao Jia, Xing Meng, Fei Huang, Lihong Dong","deadline":"2026","source":"Crossref","priority":6,"created_at":"2026-06-27T21:51:40.076393","quality_score":0,"quality_reason":""},{"id":211,"type":"publication","title":"Optimizing Visual Analytics Workflows: From Theory to Practice","institution":"OpenAlex","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,computer science,workflow,visual analytics,complement (music),ontology,data science","description":"The principle of visual analytics (VA) is to provide integrated workflows where human-centric processes (e.g., visualization and interaction) and machine-centric processes (e.g., statistics and algorithms) complement each other. To implement this principle in practice, it is necessary to reason about the trade-offs among different processes and make optimal use of them in a workflow. Building on an existing ontology of the methodology for analyzing such trade-offs information-theoretically and for optimizing VA workflows systematically, we investigate ways to transform this methodology from theory to practice. In particular, we adopted the action research method. Through case studies in different application domains, VA researchers with different background knowledge and experiences offered their answers to several hypotheses about using the methodology in practice and proposed ways forward. In this paper, we present our collective analysis, the strengths and feasibility of this theory-based methodology, as well as the obstacles to its broad deployment in practice. To address these challenges, we outline a roadmap to remove such obstacles.","url":"https://openalex.org/W7165972441","contact":"Philip Beaucamp, Alfie Abdul‐Rahman, Rita Borgo, Wolfgang Jentner, Saiful Khan, Yiwen Xing, David Ebert, Min Chen","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:18:32.932503","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1425,"type":"publication","title":"PROMOTING EFFECTIVE CURRICULUM IMPLEMENTATION IN NIGERIA THROUGH LESSON STUDY APPROACH AS A COLLABORATIVE FRAMEWORK FOR TEACHERS' PROFESSIONAL DEVELOPMENT","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,journal article","description":"Journal article. Abstract This article examines lesson study approach as a collaborative framework for strengthening teachers’ professional development and promoting effective curriculum implementation in Nigeria. The paper is situated within the context of ongoing curriculum reforms that emphasize competency-based and outcome-based learning, yet continue to face persistent implementation gaps due to inadequate teacher support, fragmented professional development, and weak interaction between curriculum policy and classroom practice. Through a critical review of relevant concepts and literature, the article argues that lesson study offers a more meaningful alternative to conventional workshop-based teacher development because it is collaborative, school-based, reflective, and grounded in real classroom inquiry. The discussion shows that lesson study approach can deepen teachers’ pedagogical knowledge, enhance professional confidence, foster collegial learning, and improve teachers’ capacity to interpret and enact curriculum goals across subject areas. It also highlights that, effective curriculum implementation depends not only on curriculum design, but on teachers’ ability to adapt instruction in response to learner needs and contextual realities. However, the article also identifies important challenges to the adoption of lesson study in Nigeria, including time constraints, weak professional culture o","url":"https://doi.org/10.5281/zenodo.20975850","contact":"GUNDE, Yakubu, DANLADI, Angbo Jatau, EWUGA, Lucky Ekka","deadline":"2026-04-01","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":923,"type":"publication","title":"Paleogeographic reconstruction of the formation of the first terrace of the Vitim River in the context of the evolution of the Mamakan Geoarchaeological Region","institution":"Irkutsk National Research Technical University, Institute of the Earth’s Crust","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,terrace (agriculture),geology,radiocarbon dating,holocene,context (archaeology),floodplain","description":"Contrary to conventional assumptions about the Holocene age of the first floodplain terrace of the Vitim River, a study of sites within the Mamakan Archaeological Ensemble (located in the lower reaches) — including Kovrizhka IV, Invalidny III (locations 3 and 4), and the Pavlova sites — reveals that the transition from floodplain to terrace occurred at varying intervals during the period 13.6–10.6 cal ka BP. These findings prompted the authors to seek an explanation and to reconstruct the history of the formation of the first terrace in relation to the location of archaeological sites. To establish a correlation between events and processes, data from a remote section of the first terrace — the Ballaganah site — were also incorporated into the analysis. This section is located 170 km upstream from the Mamakan River, on the left bank of the Vitim River. The research combined sedimentological analysis (to determine sediment genesis) and radiocarbon dating. It has been established that the final formation of the first terrace occurred at different times across the study area: at Kovrizhka IV, approximately 13.6–13.4 cal ka BP; at Invalidny III (location 4), approximately 14–13 cal ka BP; at Pavlova, approximately 11.9–10.9 cal ka BP; and on a broader scale along the Vitim River, approximately 10.6–9.6 cal ka BP. The final formation of the first terrace is associated with the completion of glacier melting and the weakening of the river's hydrological re-gime. Furthermore, records","url":"https://doi.org/10.20874/2071-0437-2026-73-2-2","contact":"A V Tetenkin, S.G. Arzhannikov, A.V. Arzhannikova, A.A. Chebotarev","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1175,"type":"publication","title":"Pan-Arctic Sea Ice Decline and Permafrost Coastal Vulnerability: An Exploratory 168-Year Assessment","institution":"Sungkyunkwan University, University of Leeds","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,arctic,sea ice,permafrost,climatology,arctic ice pack,climate change","description":"The Arctic is warming nearly four times faster than the global mean, driving unprecedented sea ice loss and threatening permafrost coasts and human settlements. Existing pan-Arctic vulnerability indices typically rest on satellite-era baselines and on expert-driven weighting schemes whose robustness is rarely tested. Here, we present an integrated, multi-centennial framework that jointly ingests SIBT1850 sea ice concentration (1850–2017), extended to 2024 with the NOAA/NSIDC Climate Data Record of Passive Microwave Sea Ice Concentration v6 (G02202 v6), together with ESA CCI Permafrost products (1997–2019), the Arctic Coastal Dynamics database, and pan-Arctic settlement inventories. Using non-parametric Mann–Kendall trend tests, Sen’s slope, and the Pettitt change point test across nine Seas (S1–S9), five permafrost-adjacent core seas exhibit summer Sen’s slopes of −0.105 to −0.185% yr−1 with Pettitt change points clustered in 1929–1953 (mean 1936), whereas three of four support seas cluster around 1978, suggesting an approximately bimodal regime shift timing that we interpret cautiously given the limited sample. A Composite Vulnerability Index integrating six normalised indicators identifies the Chukchi (CVI = 0.630) and East Siberian (0.624) seas as the highest-priority hotspots at the SIBT1850 baseline. A satellite-era robustness check using NSIDC G02202 v6 confirms that the Chukchi–East Siberian–Laptev corridor remains in the top three highest-vulnerability basins under th","url":"https://doi.org/10.3390/land15061075","contact":"Seung-Jun Lee, Jisung Kim, Hong Sik Yun","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1431,"type":"publication","title":"Parental Social Media Use and Parenting Style on Nigerian Adolescents' Identity Development and Mental Health","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,journal article","description":"Journal article. The impact of parental social media use and parenting style on the identity development and mental health of adolescents in Nigeria is conceptually examined in this research. The research examines how parents' online behaviours specifically, sharenting-influence adolescent psychological adjustment, self-perception, and social functioning, drawing on Erikson's psychosocial theory of identity formation and Baumrind's typology of parenting styles. Using a critical analysis of recent research, the conversation focusses on how, depending on the type of parental interaction and communication, digital parenting techniques can either help or hurt adolescents’ emotional resilience. The study makes the case that although social media offers chances for support and connection, it also puts young people at risk for issues including anxiety, identity confusion, and privacy violations when parents overshare their kids' personal information online. According to the study's findings, protecting adolescents’ mental health in a quickly changing digital world requires raising parental digital literacy and fostering moral online conduct. In order to preserve children's mental health, the report recommends implementing child-centred data-protection regulations, establishing consent-based internet sharing norms, and incorporating digital literacy into parenting education programmes. This package was used to process seismic data recorded on sea ice in Svalbard (Norway), in March 2019. The inversion determines the position of the icequake source and sea ice thickness. More details in: Moreau et al, Analysis of microseismicity in sea ice with deep learning and Bayesian inference: application to high-resolution thickness monitoring, The Cryosphere (2023): https://doi.org/10.5194/tc-2022-212 Updated: June 27, 2026 by the architect: Travis Raymond-Charlie Stone assisted by AI Quality Assessment APP Drink Chemistry : 1) coffee condition 2) +additives conditions Over time = Output If abstracted drug interactions can be detected: example python like react app code estimate drink temperature acidity nutrition etc. import React, { useState, useEffect } from 'react'; const ThreeBodyCoffeeApp = () => { // State for additive body // State for environmental factors Remispora maritima Linder, Farlowia 1 (3): 410 (1944) Halosphaeria maritima (Linder) Kohlm., Canad. J. Bot. 50 (9): 1956 (1972). Synonymy. Remispora lobata Höhnk, Veröff. Inst. Meeresf. Bremerhaven 3: 206 (1955). Description. Saprobic on wood. Sexual morph. Ascomata 180–570 (– 670) µm in diam., globose, subglobose, or ovoid, immersed or superficial, ostiolate, papillate, coriaceous, almost hyaline, cream-colored or smoke-gray, sometimes the upper part darker than the lower, solitary or gregarious. Peridium is 8–32 µm thick, composed of six to nine layers of thick-walled, more or less elongated cells with large lumina, forming a textura angularis, merging into the pseudoparenchyma of the venter. Necks 100–390 (– 600) × 20–60 µm, subcylindrical or truncate-conical, sometimes forked or two on one ascocarp, centric or eccentric. Pseudoparenchyma of thin-walled, large, ellipsoidal or polygonal cells filling the venter of young ascocarps; eventually breaking up into catenophyses, 7–9.5 µm in diameter. Asci 72–148 × 21.5–39 µm, 8 - spored, clavate or broadly fusoid, somewhat apiculate, pedunculate, unitunicate, thin-walled, aphysoclastic, without apical apparatuses, early deliquescing, developing at the base of the ascocarp venter. Ascospores 18&nda","url":"https://doi.org/10.5281/zenodo.20850134","contact":"Dayarathne, Monika C., Jones, E. B. Gareth, Bahkali, Ali H., Devadatha, Bandarupalli, Hyde, Kevin D., Abdel-Wahab, Mohamed A., Calabon, Mark S., Correia, Pedro","deadline":"2026-06-25","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":467,"type":"publication","title":"Reply on RC1","institution":"Institut polytechnique de Grenoble, Centre National de la Recherche Scientifique, Institut National de Recherche pour l'Agriculture, l'Alimentation et l'Environnement","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,geology,geodesy,geodetic datum,iceberg,glacier,geophone","description":"Abstract. As they reach the ocean, Antarctic outlet glaciers transition from grounded to floating at their so-called grounding lines (GL). This transition is known to be mechanically controlled by tides, which induce ice flexure visible at the surface from satellite and ground geodesy and often used as a proxy for grounding line position. Here, we use a dense seismic node array to study the spatial and temporal dynamics of surface, crevasse-induced icequake activity and basal, sliding-induced seismicity at the grounding zone of the Astrolabe Glacier, a fast-moving outlet glacier in East Antarctica. We observe that surface icequakes mimic the expected, tide-induced, ice flexure pattern, as they delineate the grounding line position inferred from previous geodetic studies, and migrate landward as tides rise. We show, however, that the mechanical grounded to floating transition is better evidenced by the spatial distribution of basal sliding-induced stick-slip events, occurring on a limited number of clusters and which depict a grounding line position that is offset inland compared to that identified from the surface. These basal events undergo tidally-driven cycles of activation and de-activation, consistent with sea water intrusion inland over at least 3 kilometers at high tides. Following these results, we propose that the monitoring of stick-slip events could be used as the most accurate means of tracking grounding line ret","url":"https://doi.org/10.5194/egusphere-2026-76-ac1","contact":"Tifenn Le Bris","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":466,"type":"publication","title":"Reply on RC2","institution":"Institut polytechnique de Grenoble, Centre National de la Recherche Scientifique, Institut National de Recherche pour l'Agriculture, l'Alimentation et l'Environnement","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,geology,geodesy,geodetic datum,geolocation,glacier,geophone","description":"Abstract. As they reach the ocean, Antarctic outlet glaciers transition from grounded to floating at their so-called grounding lines (GL). This transition is known to be mechanically controlled by tides, which induce ice flexure visible at the surface from satellite and ground geodesy and often used as a proxy for grounding line position. Here, we use a dense seismic node array to study the spatial and temporal dynamics of surface, crevasse-induced icequake activity and basal, sliding-induced seismicity at the grounding zone of the Astrolabe Glacier, a fast-moving outlet glacier in East Antarctica. We observe that surface icequakes mimic the expected, tide-induced, ice flexure pattern, as they delineate the grounding line position inferred from previous geodetic studies, and migrate landward as tides rise. We show, however, that the mechanical grounded to floating transition is better evidenced by the spatial distribution of basal sliding-induced stick-slip events, occurring on a limited number of clusters and which depict a grounding line position that is offset inland compared to that identified from the surface. These basal events undergo tidally-driven cycles of activation and de-activation, consistent with sea water intrusion inland over at least 3 kilometers at high tides. Following these results, we propose that the monitoring of stick-slip events could be used as the most accurate means of tracking grounding line ret","url":"https://doi.org/10.5194/egusphere-2026-76-ac2","contact":"Tifenn Le Bris","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1243,"type":"publication","title":"Representing glacier evolution for modelling hydrological responses to climate change in mountainous catchments","institution":"Journal of Hydrology","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":"Crossref publication metadata. Journal: Journal of Hydrology. Authors: Denis Ruelland, Florian Antoine, Antoine Rabatel. Year: 2026.","url":"https://doi.org/10.1016/j.jhydrol.2026.135769","contact":"Denis Ruelland, Florian Antoine, Antoine Rabatel","deadline":"2026","source":"Crossref","priority":6,"created_at":"2026-06-27T21:51:40.076393","quality_score":0,"quality_reason":""},{"id":1402,"type":"publication","title":"Resolving subglacial hydrology network dynamics through seismic observations on an Alpine glacier.","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,other,cryoseismology,subglacial hydrology,glacier","description":"Other. This is my PhD manuscript on " Resolving subglacial hydrology dynamics through seismic observations on an Alpine glacier ". This file can be also uploaded from: https://hal.univ-grenoble-alpes.fr/tel-03191311v1. You can also find my PhD presentation PDF and the associated video can be found here or copy/paste this link: https://www.youtube.com/watch?v=IuEv7JKiYrg&t=475s or search for Ugo Nanni on youtube. Summary: The way in which water flows in the subglacial environment exerts a major control on ice-bed mechanical coupling, which strongly defines glacier sliding speeds. Today our understanding on the physics of the subglacial hydrology network is limited because of the scarcity of field measurements that yield a partial representation of the heterogeneous subglacial environment. The aim of my PhD work is to use passive seismology to help overcome common observational difficulties and quantify the evolution of the subglacial hydrology network pressure conditions and its configuration. Recent works show that subglacial turbulent water flow generates seismic noise that can be related to the associated hydrodynamics properties. These analyses were conducted over a limited period of time making it unclear whether such approach is appropriate to investigate seasonal and diurnal timescales,","url":"https://doi.org/10.5281/zenodo.4683985","contact":"Nanni, Ugo","deadline":"2020-12-03","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":468,"type":"publication","title":"Resources for the REASSESS paper on Low Frequency Icequakes during cavity drainages","institution":"Institut polytechnique de Grenoble, Centre National de la Recherche Scientifique, Institut National de Recherche pour l'Agriculture, l'Alimentation et l'Environnement, GFZ Helmholtz Centre for Geosciences, Aberystwyth University, University of Sheffield","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,geology,python (programming language),seismology,water level,gnss applications,remote sensing","description":"This dataset contains data and codes used for the paper \"Low frequency icequakes generated during transient cavity drainage on a Greenlandic outlet glacier\". Following files are provided: GNSS F an G data (24.catv.XYZ.ISF0.bu6.ma6.combined.csv and 24.catv.XYZ.ISG0.bu6.ma6.combined.csv) MFP localizations for frequency range 1.5-21 Hz and 4-6Hz (event_list_1.5_2.1Hz.csv and event_list_4_6Hz.csv) Water routing (hydraulic_potential_acc_k1.050_3413.tif) and hydro-potentials (hydraulic_potential_k1.050_3413.tif) seismic signal station F (stationF.csv) contour of the lakes (Lakes.mat) node positions (pos_nodes_oct-LAT-LON.csv) on map photoaerienne_reseau_2024.tif Ice thickness (icethick_kriging_res20_methodLINEAR_lag4.tif) families of surface events correlated_families_SurfaceSources.csv families of deep events: correlated_families_1_DeepSources.csv and correlated_families_2_DeepSources.csv The MSEED seismic files of each nodes for the 10th, 11th and 12th of September 2024. Downsampled to 200Hz.-> MSEED_downsampled.zip All this data can be used with the provided Python code, which corresponds to the code used to generate the respective figures in the paper: Figure1.py, Figure2a.py, Figure2def.py and Figure3.py","url":"https://doi.org/10.5281/zenodo.20728994","contact":"Hugo Rousseau, Florent Gimbert, Jules Le Bot, Reza Esfahani, Samuel Doyle, Nicolas Paris, Michel Campillo, Stephen J. Livingstone","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":293,"type":"publication","title":"Revisiting the “Asiatic Mediterranean”: Early Holocene highstands and hydrological connectivity across the Ponto-Caspian basin","institution":"OpenAlex","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,geology,holocene,structural basin,quaternary,climatology,climate change","description":"Understanding hydrological change across the Ponto-Caspian region during the Late Pleistocene-Early Holocene transition remains a key challenge in Quaternary science.While existing models emphasise climate forcing and glacio-isostatic adjustment, a number of geomorphological, sedimentary, and biological observations are not easily reconciled within current frameworks.This study synthesises evidence from the Caspian, Black Sea, Mediterranean, and adjacent regions, with particular focus on the geomorphology of Azerbaijan.Raised terraces, high-elevation strandlines, and apparent wave-modified mud-volcano surfaces occur at levels significantly above the widely accepted Khvalynian highstand (~+50 m a.s.l.), suggesting the possibility of previously unrecognised hydrological conditions.Additional lines of evidence include ostracod faunal turnovers, shifts in salinity-sensitive taxa, anomalous sedimentary records, and indications of changing basin connectivity across Eurasia during the Early Holocene.Taken together, these observations support the interpretation that regional hydrology was more dynamic and complex than commonly assumed.Rather than a single-event framework, the data are more consistent with a multi-phase system involving fluctuating water levels, episodic basin overspill, stratified flow regimes, and variable connectivity between the Black Sea, Caspian Sea, and neighbouring basins.In this context, earlier concepts of an enlarged Pleistocene \"Asiatic Mediterranean\" are ","url":"https://doi.org/10.35714/ggistrat20260100021","contact":"R. Gallagher","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:18:32.932503","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1190,"type":"publication","title":"Rising tides: Unveiling the spatial and temporal evolution of sea level rise under climate change","institution":"The University of Melbourne, Wuxi Taihu Hospital, Hohai University","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,hotspot (geology),climate change,climatology,sea level,environmental science,sea level rise","description":"This study systematically investigates the spatiotemporal evolution of sea level rise under climate change, employing a tri-scale quantitative framework (global, China's coastal waters, and Shanghai municipality) to elucidate its underlying drivers and regional disparities. By synthesizing IPCC AR6 datasets and NASA sea level projection models, we integrate the Theil-Sen Median Method with Mann-Kendall Test to analyze trajectory patterns from 2030 to 2100. Spatial clustering effects are further identified through hotspot analysis (Getis-Ord Gi*) implemented in ArcGIS Pro. The findings reveal a statistically significant upward trend in global sea levels, primarily attributed to thermal expansion and cryospheric melt (glaciers and polar ice sheets), with localized subsidence observed in certain high-latitude regions. China's coastal waters exhibit accelerated sea level rise, particularly in the South China Sea and East China Sea, where rates surpass the global mean-a phenomenon driven by coupled effects of monsoon circulation, Kuroshio Current dynamics, and freshwater discharge from major rivers (e.g., Yangtze and Yellow Rivers). At the urban scale, Shanghai's coastal zone demonstrates exacerbated relative sea level rise due to superimposed land subsidence and localized hydrodynamic processes, manifesting distinct spatiotemporal clustering patterns. By integrating global-scale thermodynamic baselines, regional oceanic drivers, and local land subsidence patterns, this study prov","url":"https://doi.org/10.1371/journal.pone.0347855","contact":"Bing Liang, Guoqing Shi, Yuxuan Zhu, Yuexi Wu, Mark Wang","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1268,"type":"publication","title":"Role of cellular austenite on fracture resistance in additively manufactured 18Ni(300) steel","institution":"Journal of Materials Science & Technology","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":"Crossref publication metadata. Journal: Journal of Materials Science & Technology. Authors: Jingtao Tang, Wenhua Wu, Wujun Yin, Guofeng Zhang, Jiongfei Zhao, Shichao Liu, Yuming Fu, Hang Yang. Year: 2027.","url":"https://doi.org/10.1016/j.jmst.2026.04.011","contact":"Jingtao Tang, Wenhua Wu, Wujun Yin, Guofeng Zhang, Jiongfei Zhao, Shichao Liu, Yuming Fu, Hang Yang","deadline":"2027","source":"Crossref","priority":6,"created_at":"2026-06-27T21:51:40.076393","quality_score":0,"quality_reason":""},{"id":1433,"type":"publication","title":"SR2609 Cruise Report","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,report","description":"Report. This is a cruise report for cruise SR2609 aboard RV Sally Ride on May 22 - June 3, 2026. This served as the recovery cruise for an Internal Wave Resolving (IWR) Array located in the North Pacific Ocean south of the Aleutian Islands as part of the National Ocean Partnership Program (NOPP) Global Internal Wave (GIW) study as part of a project called “A Distributed Network of Internal Wave Resolving Moored Arrays for Assessing Tide-Resolving Model Fields and Improving Forecasts in the Coastal Ocean.” Abstract This study examined secondary school students’ interest in Biology when taught using the 7E instructional model and the conventional teaching method, with emphasis on gender and school location in Bayelsa State. A quasi-experimental pre-test, post-test, non-equivalent control group design was adopted for the study. The population comprised all Senior Secondary School II Biology students in public secondary schools in Bayelsa State, while a sample size of two hundred and thirty-eight Biology students drawn from selected co-educational secondary schools in Yenagoa Local Government Area was used. Intact classes were assigned to experimental and control groups through balloting, and instruction was delivered by regular Biology teachers who were trained as research assistants prior to the treatment. Data were collected using the Biology Interest Inventory, and the reliability of the instrument was established using the Cronbach alpha method. Two research questions and two null hypotheses guided the study. Mean and standard deviation were used to answer the research questions, while Analysis of Covariance was employed to test the hypotheses at the 0.05 level of significance. The findings revealed that although male students recorded slightly higher mean post-test mean interest scores than female students across the two inst","url":"https://doi.org/10.5281/zenodo.20976603","contact":"EGBULONU, Emelda Ugochi, ADATA, Dickson Theophilus Diepiribo","deadline":"2026-04-01","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":992,"type":"publication","title":"Salix polaris growth rings are an unreliable proxy for satellite-derived tundra productivity on Svalbard","institution":"Wageningen University & Research","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,tundra,proxy (statistics),productivity,environmental science,physical geography,climatology","description":"The Arctic is warming nearly four times faster than the global average, with Svalbard among the regions experiencing the most extreme warming. This has likely driven widespread “greening” of the archipelago, yet in-situ data on tundra productivity in Svalbard remain scarce, and satellite-based measurements are challenged by cloud cover and low sun angles. This study assessed whether Salix polaris growth ring width can serve as a proxy for large-scale tundra productivity on Svalbard, quantified using NDVI. The results indicate that S. polaris growth rings are not a reliable indicator, as only two of nine sites returned a significant (p ' 0.05) ring width-NDVI relationship, associations across sites were very weak (R2 ' 0.05), and predictive performance of ring-width timeseries for local interannual tundra NDVI based on unseen sites was very poor (Nash-Sutcliffe Efficiency ' −2). These findings contrast with studies on other Salix species and small-scale biomass changes. S. polaris radial growth increased with summer temperature and thawing degree-days but decreased with freezing degree-days and delayed snowmelt at multiple sites, while other climatic effects were site-specific. NDVI responded more consistently to climate, increasing with summer temperature, thawing degree-days, and summer precipitation, and decreasing with delayed snowmelt and winter precipitation. Differences in how S. polaris radial growth and NDVI respond to climate, along with the influence of abundant non","url":"https://doi.org/10.1016/j.dendro.2026.126538","contact":"Tom Verstraten, Harm Bartholomeus, Rúna Í. Magnússon","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":559,"type":"publication","title":"Sea-level contribution from Thwaites Glacier doubles in an observation-constrained ice-sheet model","institution":"University of California, Irvine, Dartmouth College, Dartmouth Hospital, University of California, Los Angeles, University of California San Diego, Jet Propulsion Laboratory","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,geology,glacier,sea level rise,sea level,lead (geology),glacial period","description":"Publication from OpenAlex. Authors: Mattia Poinelli, Eric Rignot, Hélène Seroussi, Josh Cuzzone, Tyler Pelle, Eric Larour. Year: 2026","url":"https://doi.org/10.21203/rs.3.rs-9216227/v1","contact":"Mattia Poinelli, Eric Rignot, Hélène Seroussi, Josh Cuzzone, Tyler Pelle, Eric Larour","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":78,"quality_reason":"priority=6, has_url, trusted_source, good_description, good_tags, has_contact_or_authors"},{"id":751,"type":"publication","title":"Seasonal glacier motion variations and underlying hydro-mechanical processes at Glacier d'Argentière, French Alps","institution":"Institut polytechnique de Grenoble, Centre National de la Recherche Scientifique, Institut National de Recherche pour l'Agriculture, l'Alimentation et l'Environnement, Institut des Sciences de la Terre, Université Gustave Eiffel","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,glacier,geology,meltwater,geomorphology,tidewater glacier cycle,glacier mass balance","description":"Abstract. Subglacial hydrology controls basal sliding of hard-bedded glaciers by modulating basal drag through changes in ice–bed separation. Yet, the underlying mechanisms that control ice–bed separation and its links with basal friction remain poorly understood. In this study, we contribute to a better understanding of this problem by evaluating spatial and temporal changes in bed separation in relation to changes in glacier horizontal velocity using three years of continuous and dense GPS records from Glacier d'Argentière (French Alps). We confirm a previous study showing that spatial and temporal variations in glacier vertical motion mainly reflect changes in ice–bed separation, as they cannot be explained by variations in internal strain rates. We find that the rate of uplift is in anti-phase with subglacial water discharge, being positive in winter in the absence of surface melt and negative during summer melt. We suggest that this behavior results from basal cavities being weakly connected in winter, allowing them to fill slowly under low water input from englacial storage release or basal melt, and then rapidly transitioning to a connected state in summer, enabling efficient drainage of surface meltwater and reduced cavity sizes. A key finding is that changes in horizontal velocity are well correlated, both in time and space, with changes in ice–bed separation. This results in an increase in horizontal velocity in winter that can be quantitatively compared with modele","url":"https://doi.org/10.5194/tc-20-3257-2026","contact":"Anuar Togaibekov, Adrien Gilbert, F Gimbert, Andréa Walpersdorf","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":738,"type":"publication","title":"Sedimentary ancient DNA records climate change and permafrost thaw effects on Arctic coastal ecosystems in the Mackenzie Delta, Canada","institution":"OpenAlex","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,permafrost,arctic,climate change,holocene,ecosystem,arctic ecology","description":"Unprecedented rates of warming are shaping Arctic ecosystems and landscapes. Impacts in the Canadian Arctic are closely connected to accelerated permafrost thaw, coastal erosion and increasing river discharge to the coastal zone. Significant shifts in biodiversity and environments are evident today, but long-term ecosystem responses are crucial for discerning the effects of Holocene climate variability and accelerating rates of change in the 21st century. Here we explore ancient DNA records from sediment records taken in Tuktoyaktuk harbor (NWT), and additional sites in front of the wider Mackenzie Delta. We applied plant and animal metabarcoding, together with shotgun metagenomics. The 4500-year harbor record reflects the region’s terrestrial and marine biodiversity at multi-decadal resolution, with distinct community shifts in particular in response to sea level rise. The identification of woolly mammoth DNA in surface sediments suggests reworking of formerly buried material from mainland permafrost into coastal sediments. We hypothesize that ‘modern’ signals of extinct megafauna may act as a proxy for accelerated permafrost thaw in response to recent warming. Our study offers new perspectives on Arctic ecosystem sensitivity to climate change across the land-sea interface, and a framework for the interpretation of sedimentary ancient DNA in a rapidly warming Arctic landscape.","url":"https://openalex.org/W7165098430","contact":"Inda Brinkmann, Julie Lattaud, Blanda Matzenbacher, Bennet Juhls, Matt O'Regan, Michael Fritz, Lisa Bröder, Tommaso Tesi","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1296,"type":"publication","title":"Seismic performance of prefabricated stainless steel-composite material non-buckling restrained braces","institution":"Case Studies in Construction Materials","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":"Crossref publication metadata. Journal: Case Studies in Construction Materials. Authors: Lina Zong, Jun Zhao, Wei Chen, Yang Peng, Hai Fang, Jun Dong. Year: 2026.","url":"https://doi.org/10.1016/j.cscm.2026.e06194","contact":"Lina Zong, Jun Zhao, Wei Chen, Yang Peng, Hai Fang, Jun Dong","deadline":"2026","source":"Crossref","priority":6,"created_at":"2026-06-27T21:51:40.076393","quality_score":0,"quality_reason":""},{"id":1292,"type":"publication","title":"Seismic response analysis of graphite core structures by 3D-DIC system","institution":"Annals of Nuclear Energy","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":"Crossref publication metadata. Journal: Annals of Nuclear Energy. Authors: Tianbao Lan, Zedong Wang, Siqi Zhu, Wei Tan. Year: 2026.","url":"https://doi.org/10.1016/j.anucene.2026.112546","contact":"Tianbao Lan, Zedong Wang, Siqi Zhu, Wei Tan","deadline":"2026","source":"Crossref","priority":6,"created_at":"2026-06-27T21:51:40.076393","quality_score":0,"quality_reason":""},{"id":1287,"type":"publication","title":"Seismic response prediction of wind turbine towers using a Bayesian framework based on chaotic map-based particle swarm optimized particle filter","institution":"Reliability Engineering & System Safety","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":"Crossref publication metadata. Journal: Reliability Engineering & System Safety. Authors: Qianqian Ren, Xiaoyang Feng, Yuefeng Kou, Qingqing Chen, Yazhou Xu. Year: 2027.","url":"https://doi.org/10.1016/j.ress.2026.113045","contact":"Qianqian Ren, Xiaoyang Feng, Yuefeng Kou, Qingqing Chen, Yazhou Xu","deadline":"2027","source":"Crossref","priority":6,"created_at":"2026-06-27T21:51:40.076393","quality_score":0,"quality_reason":""},{"id":1290,"type":"publication","title":"Seismic wave propagation and multi-supported underground seismic motions in submerged seasonally frozen soil","institution":"Applied Mathematical Modelling","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":"Crossref publication metadata. Journal: Applied Mathematical Modelling. Authors: Guohuan Liu, Xinyang Li. Year: 2026.","url":"https://doi.org/10.1016/j.apm.2026.117115","contact":"Guohuan Liu, Xinyang Li","deadline":"2026","source":"Crossref","priority":6,"created_at":"2026-06-27T21:51:40.076393","quality_score":0,"quality_reason":""},{"id":1401,"type":"publication","title":"Seismological monitoring of Svalbard's cryosphere: current status and knowledge gaps","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,report,Seismology,glaciology,calving,monitoring,ice-quake,permafrost","description":"Report. This is chapter 5 of the State of Environmental Science in Svalbard (SESS) report 2019 (https://sios-svalbard.org/SESS_Issue2). The new research field of cryoseismology studies ground shaking (seismic waves) generated in the frozen part of our planet. The shaking is caused by processes such as icequakes related to the movement of glaciers, glacier calvings, and flowing meltwater. Climate change affects processes at glaciers such as calving and causes changes in the permanently frozen ground (permafrost) in polar regions. Cryoseismology can measure these changes using seismic waves. Accessibility and well-developed logistics mean that Svalbard is much easier to work in than other regions in the Arctic or the Antarctic, and make Svalbard a natural laboratory to study changes in the cryosphere induced by climate change. Continuous seismic data collection in Svalbard (going back as long as decades) allows us to observe long-term trends and changes in seasonal patterns of glacial seismicity or sub-surface structures (permafrost). High temporal resolution of seismic data provides much more detail, e.g. about the calving process, than satellite images and helps us estimate the mass of ice that glaciers lose due to calving. Strong calving in Svalbard can be registered at great distances (up to 100 km) and measurements are fully independent of visibility, which allows for observation of calving regardless o","url":"https://doi.org/10.5281/zenodo.4704584","contact":"Köhler, Andreas, Gajek, Wojciech, Malinowski, Michal, Schweitzer, Johannes, Majdanski, Mariusz, Geissler, Wolfram H, Chamarczuk, Michal, Wuestefeld, Andreas","deadline":"2020-01-13","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":1456,"type":"publication","title":"Short-range diversity and invasion dynamics of the freshwater jellyfish Craspedacusta sowerbii in Lake Kinneret, Israel, and its watershed: field sampling combined with hydrodynamical simulations","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,journal article,Cnidaria,COI,hydrodynamical simulations,invasion genetics,Lagrangian particle tracking","description":"Journal article. The hydrozoan Craspedacusta sowerbii, native to the Yangtze River system in China, has become an invasive species in freshwater ecosystems worldwide. Multiple genetic lineages have been introduced globally, yet the species' taxonomic identity has not been comprehensively resolved. The species life cycle alternates between a benthic polyp stage and a pelagic medusa stage, the latter being the primary focus of most distributional studies. In Israel, the species was previously reported from the Lake Kinneret watershed, though recent records are lacking. Here, we surveyed streams and ponds in the Golan Heights for both medusae and polyps and conducted genetic analyses on collected specimens. Three distinct cytochrome c oxidase subunit I (COI) haplotypes were identified, corresponding to those previously described from European and Asian populations. Most sites exhibited homogeneous COI haplotype composition, apart from a single site where different COI haplotypes co-occurred. This pattern suggests restricted short-distance dispersal and exchange, consistent with multiple independent colonization events. While our survey did not confirm the presence of C. sowerbii in its pelagic stage, the detection of polyps in multiple inflowing streams suggests that colonization of Lake Kinneret itself is likely in the future. To facilitate a proper monitoring program, we simulated the movement and distribution of possible medusae aggregations, originating from","url":"https://doi.org/10.3897/neobiota.107.179109","contact":"Dehos, Stefan, Amitai, Yael, Kuplik, Zafrir, Sussholz, Noy, Gießler, Sabine, Stibor, Herwig, Heifetz, Eyal","deadline":"2026-06-24","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":1471,"type":"publication","title":"Signa: automatic ArUco ground control point detection for WebODM","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,software,WebODM,OpenDroneMap,ArUco,ground control points,photogrammetry,georeferencing,archaeology,reproducible research software","description":"Software. Signa is a WebODM plugin for automatic ArUco ground-control-point (GCP) detection. It detects ArUco markers in a photogrammetry task's images, matches them against measured GCP coordinates, and produces an OpenDroneMap-compatible gcp_list.txt for single-pass georeferencing of (archaeological) drone surveys, server-side inside WebODM with no command line.","url":"https://doi.org/10.5281/zenodo.20856248","contact":"Leiverkus, Patrick","deadline":"2026-06-25","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":724,"type":"publication","title":"Simulating jökulhlaups from an ice-marginal lake within a 2D model of subglacial drainage and basal sliding","institution":"Aberystwyth University, Northumbria University, Institute of Geography, Dartmouth College, University of Bristol, Durham University","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,geology,glacier,geomorphology,drainage,glaciology,hydrology (agriculture)","description":"Abstract. Ice-marginal lakes are an increasingly common feature of glacierised landscapes, and their sudden drainage beneath glaciers (a jökulhlaup) can threaten downstream communities and infrastructure. Numerous efforts to model jökulhlaups have been made, however, because these models are 1D representations of a single channel connected to a lake, they cannot simulate lateral jökulhlaup propagation through the subglacial system. Here, to simulate jökulhlaups within a 2D subglacial drainage system, we use a fully coupled model of subglacial hydrology and basal sliding with a time-evolving ice-marginal lake located at its boundary. In experiments on a synthetic domain, the model produces stable, recurrent jökulhlaup cycles, and glacier acceleration during flood onset followed by abrupt slowdown at peak flood discharge. Sensitivity testing highlights the efficiency of the subglacial hydrology system as a key control on flood timing, peak discharge, and the basal sliding response. We also explore our model’s ability to represent an observed record of jökulhlaups by applying it to Isunnguata Sermia, West Greenland. The model successfully reproduces variability over a 17-year period, but underpredicts peak flood discharges, likely because its formulation omits ice uplift and lake temperature variability. These results establish the coupling of a lake to 2D subglacial hydrology and ice dynamics as a viable approach for multi-decadal jökulhlaup simulation.","url":"https://doi.org/10.5194/egusphere-2026-2948","contact":"Adam Hepburn, Sammie Buzzard, Andrew Sole, Stephen J. Livingstone, Felix Ng, Mathieu Morlighem, Elizabeth Bagshaw, Caroline Clason","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":776,"type":"publication","title":"Simulating meltwater oxygen isotopes as a proxy for assessing geothermal heat flow in Greenland","institution":"Australian Antarctic Division, University of Bergen, Centre National de la Recherche Scientifique, Météo-France, Bavarian Academy of Sciences and Humanities, Bjerknes Centre for Climate Research, Earth Science Institute of the Slovak Academy of Sciences","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,meltwater,geothermal gradient,geology,greenland ice sheet,geothermal heating,ice sheet","description":"Geothermal heat flow is an important control on the dynamics of glaciers and ice sheets. In Greenland however, the exact magnitude and distribution of geothermal heat flow under the ice sheet is largely unknown as only few direct measurements exist at the locations of the deep ice cores. For this reason, several studies have attempted to constrain geothermal heat flow under the ice sheet through various statistical, geophysical, and ice-dynamical modelling efforts. However, many of the different heat flow estimates produced by these models disagree substantially in terms of magnitude and spatial distribution of estimated heat flow values. The oxygen stable isotope composition of ice sheet basal meltwater has so far not been considered in studies of Greenland geothermal heat flow. In this study, we simulate how different estimates of geothermal heat flow affect the production of basal meltwater and its isotopic composition. In our simulations, the modelled Öz Bu kuramsal makale, yapay zekâ ajan/personalarının sosyal medyada “kullanıcı gibi” katılımının, insan üretimi üslup, içerik ve öz-sunum pratiklerinde taklit temelli yakınsamayı nasıl tetiklediğini ele alır ve bu ilişkiyi Çift Yönlü Mimesis Döngüsü (ÇYMD) çerçevesiyle kavramsallaştırır. Önerdiğimiz Çift Yönlü Mimesis Döngüsü (ÇYMD), (i) insan üretiminden öğrenen ve onu taklit eden ajanların, (ii) platform metriklerinin (beğeni, izlenme, öneri sinyalleri) sağladığı geri bildirimle çıktılarının optimize edilmesi ve (iii) bu optimize kalıpların insan yaratıcılar tarafından geri taklit edilmesi süreçlerinin kapanan bir çevrim oluşturduğunu ileri sürer. Çerçevede, Metrik Baskısı (kamusal geri bildirim görünürlüğü ve temposu) döngünün ivmesini (kazanç) ve tonunu (düzleştirici/steril vs. uçlaştırıcı/kutuplaştırıcı) belirleyen bir modülatör olarak konumlandırılır. Böylece ajan katılımı yalnızca içerik hacmini artırmakla kalmaz; dilsel, biçimsel ve duygusal düzeyde standartlaştırıcı bir kuvvet üretebilir. Sınır koşulları olarak vernaküler yaratıcılık, parodi, niş topluluk normları ve etiketleme/a&cce","url":"https://doi.org/10.5281/zenodo.20962662","contact":"Eser, Oğuz Ömer","deadline":"2026-06-27","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":1283,"type":"publication","title":"Spatial Variation of Seismic Energy Release of Himachal Pradesh","institution":"Disaster Advances","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":" The supplementary material contains three videos of fragment observations from two events: two videos from Iceland on 21 October 2023 near Guesthouse Brekka, south of Húsavík, recorded by Olivier Staiger, and one video from Antarctica on 9 June 2019 near the geographic South Pole, recorded by Benjamin Eberhardt. One Iceland file is a real-time video recorded with a handheld Sony a7s2 camera from 05:40 to 05:42 UTC. The other Iceland file is a timelapse video recorded with a Canon EOS R-series camera from 05:10 to 06:06 UTC. The real-time video was recorded at 25 fps, while the timelapse video was assembled from 811 individual images into a 30 fps video. The Antarctica file is a segment from a 25-hour timelapse recording observed between 03:20 and 05:00 UTC near the South Pole Telescope, recorded at 25 fps with a Sony ILCE-7RM3 camera on a motorised tripod. Soy milk ice cream is an alternative food product for those with lactose intolerance who cannot consume cow's milk. The addition of cashew nut puree increases the fat content and improves the texture of the ice cream, making it smoother and creamier. This study aims to determine the effect of variations in cashew nut puree concentration on the physicochemical and organoleptic properties of soy milk ice cream. This study used a laboratory experimental method with a completely randomized design (CRD) with one factor consisting of four treatment levels, namely the addition of cashew nut puree of 0%, 10%, 20%, and 30%, each with three replications . The parameters observed included physicochemical properties consisting of protein, fat, overrun, melting speed, total solids, and organoleptic tests (color, aroma, taste, and texture). The results showed that the addition of cashew nut puree had a significant effect (p <0.05) on the physicochemical and organoleptic properties of soy milk ice cream. The treatment with the addition of 30% cashew nut puree showed the highest values in protein, fat, and total solids levels, and produced a slower melting speed and a higher level of sensory acceptance compared to other treatments. Although the highest overrun value was obtained in the treatment with the addition of 20% cashew nut puree, increasing the concentration of cashew nut puree to 30% generally resulted in an increase in the physicochemical quality and organole","url":"https://doi.org/10.5281/zenodo.20952032","contact":"Audry Azzahra ikhsan, Kejora Handarini, Retnani Rahmiati, Dewi Mariyanah","deadline":"2026-02-28","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":1221,"type":"publication","title":"Taxonomy and molecular evaluation of the Halosphaeriaceae (Microascales, Hypocreomycetidae)","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,journal article,Ascomycota,ecology,life below water,new taxa,marine,Sordariomycetes,taxonomy","description":"Journal article. This study re-evaluates the classification of the Halosphaeriaceae (Microascales, Hypocreomycetidae) based on phylogenetic analyses of 18S and 28S regions of rDNA and protein coding genes (rDNA, RPB1, RPB2, TEF1-ɑ, MCM7) along with comprehensive morphological comparisons. Halosphaeriaceae are worldwide in distribution and commonly found in marine habitats. A natural classification was not possible when the family was introduced, since it predated molecular phylogenetic studies; therefore, morphology-based descriptions only were provided. This study recognises 77 genera with 202 species which includes seven new genera (Neoaniptodera, Neogesasha, Neohalosarpheia, Pangia, Remisporiopsis, Sheareromyces, Shiiraspora), and one new species Ocostaspora japonica. The new taxonomic combinations include Halosarpheia australiensis, Halosphaeriopsis alopallonella, Neoaniptodera juncicola, Neogesasha mangrovei, Neohalosarpheia marina, Pangia limnetica, Remisporiopsis macrocephala, R. quadri-remis, R. spitsbergenensis, R. stellatus, R. submersa, Sheareromyces aquibella, Shiiraspora salsuginosa and Thalassogena unicellularis. Divergent time estimation of Halosphaeriaceae, based on combined 18S, 28S rDNA, RPB1, RPB2, TEF1-ɑ, MCM7 sequences, indicates that the family originated in the Paleozoic at ~545 MYA. Ecologically, H","url":"https://doi.org/10.3897/mycokeys.135.187540","contact":"Dayarathne, Monika C., Jones, E. B. Gareth, Bahkali, Ali H., Devadatha, Bandarupalli, Hyde, Kevin D., Abdel-Wahab, Mohamed A., Calabon, Mark S., Correia, Pedro","deadline":"2026-06-25","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:44:55.032906","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":624,"type":"publication","title":"Technical note: A new monitoring approach to measure water vapor isotopes in high altitude regions","institution":"Indian Institute of Technology Delhi, Desh Bhagat University, University of Bern, Oeschger Centre for Climate Change Research","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,environmental science,water vapor,calibration,effects of high altitude on humans,meteorology,moisture","description":"Abstract. Water vapor isotopes provide a comprehensive perspective on the moisture source dynamics for tracing the physical processes in hydrological and climatic studies. Continuous real-time water vapor isotopic measurements using Cavity Ring-Down Spectroscopy (CRDS) techniques are mostly based at stations located in high latitudes and the low-lying tropical regions. Such investigations from high-altitude, tropics, subtropical – mid-latitude transition zone – the Himalayas is limited owing to challenging physical conditions and multiple forms of precipitation occurring in the region. In this study, we report the establishment of the first continuous high-altitude isotope-monitoring laboratory in Northwest Himalayas windward side Manali (2,050 above msl) and leeward side Sissu (3,120 above msl) using the Picarro L2140-i Cavity Ring-Down Spectroscopy (CRDS) analyzer. This instrument enables real-time measurements of δ¹⁷O, δ¹⁸O, and δ2H in local atmospheric water vapor. Our laboratory setup integrates installation of Picarro analyzer, a heating air inlet system, meteorological sensor, lightning arrester and calibration protocols suited for optimum performance of the instrument in such challenging high-altitude Himalayan environment. Our laboratory setup protocols integrate the best practice and published guidelines with some additional modifications to mitigate the challenges in water vapor isotopic measurements in high altitude environment. A limitation of the current dataset","url":"https://doi.org/10.5194/egusphere-2026-220","contact":"G Kiran Kumar, Yama Dixit, Anubhav Singh, Shyam Ranjan, Markus Leuenberger","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1473,"type":"publication","title":"Temporal-relations","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,software,Chronology,Archaeology,Computational archaeology","description":"Software. Code of the revised preprint version of the article \"Detecting Temporal Relations in Archaeology: Model and Algorithms\", after first round of peer-review.","url":"https://doi.org/10.5281/zenodo.20849142","contact":"Levy, Eythan","deadline":"2026-06-25","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":937,"type":"publication","title":"Testing current estimates of the in situ cosmogenic 10 Be production rate in the north-western British Isles, with implications for ice sheet behaviour during Termination 1","institution":"Ollscoil na Gaillimhe – University of Galway, University of Maine, University of Cincinnati","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,cosmogenic nuclide,surface exposure dating,geology,calibration,radiocarbon dating,physical geography","description":"Abstract. Cosmogenic nuclide surface-exposure dating (SED) is a rapidly growing tool in geoscience owing to its unrivalled potential for directly dating rock surfaces and thus the geomorphic and climatic events they represent. Fundamental to the efficacy of the SED method is reliable constraint of the in situ production rate, which is typically calculated via calibration experiments: cosmogenic nuclide concentrations are measured in surfaces for which the true exposure age is known independently, allowing the production rate to be derived (in atoms g−1 yr−1) for the specific calibration site. This value can then be extrapolated to distal field sites using numerical scaling methods designed to account for spatial and elevational differences in geomagnetic and atmospheric shielding. Thanks to successive and increasingly co-ordinated calibration efforts, production rate estimates for the most widely used cosmogenic nuclide, beryllium-10 (10Be), have improved in recent decades, with the majority converging on sea-level high-latitude (SLHL) values of ∼ 3.8–4.1 atoms g−1 yr−1 (“St” scaling). Nonetheless, there remains sufficient variability among production rates to undermine the reliability of derived surface-exposure ages, particularly for applications to short-lived events such as the abrupt climate shifts of the last glacial termination. To help address this uncertainty, this paper reports new 10Be concentrations from deglacial surfaces on the Redpoint Peninsula in north-west S","url":"https://doi.org/10.5194/gchron-8-329-2026","contact":"Gordon Bromley, Brenda L. Hall, Aaron E. Putnam, Thomas V. Lowell","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":839,"type":"publication","title":"The Development of a Low Power GNSS System, as Part of a Drone Assisted Environmental Sensor Network for a Glacial Environment","institution":"University of Southampton, PragmatIC (United Kingdom), University of Bologna","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,drone,gnss applications,glacier,remote sensing,real-time computing,computer science","description":"Abstract We show the development of an innovative Internet of Things Real Time Kinematic Global Navigation Satellite System, to study the short‐term changes in surface velocity of two adjacent Icelandic glaciers, in order to understand the response of glaciers to climate change. We show for the first time that we are able to deploy such a system using an Uncrewed Aerial Vehicle, which allows inaccessible areas of the glacier to be studied. This system is low power, cost effective, with centimeter‐level accuracy and transmits its data to the web server daily. Whilst there were variations in transmission success, overall our data indicate clear similarities in temporal velocity variations between the rovers at the individual sites, both at Breiðamerkurjökull where the rovers were only ∼200 m apart as well as Fjallsjökull where they were ∼1 km apart. This demonstrates how velocity patterns (but not magnitudes) were similar across the glacier.","url":"https://doi.org/10.1029/2025ea004549","contact":"K. Martinez, Sherif Attia, Graeme M. Bragg, A. Andrews, N. R. Baurley, J. K. Hart","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":342,"type":"publication","title":"The Effect of Topological Defects and Magnetic Flux on Fully-Heavy Tetraquarks and Mass Spectra of Heavy Quarkonia Using the Analytical Exact Iteration Method","institution":"arXiv","country":"International","city":"","latitude":null,"longitude":null,"tags":"arxiv,publication,preprint","description":"Investigating the non-perturbative behavior of QCD and the dynamics of strong interaction is crucial for the study of heavy quarkonia and the understanding of exotic fully-heavy tetraquarks. In this work, using the analytical exact iteration method (AEIM), the analytical eigenvalue solutions of the non-relativistic Schrödinger equation are obtained in the presence of topological defects and external magnetic flux. The interactions are modelled using a modified Cornell potential supplemented by harmonic and inverse quadratic terms. We demonstrate that the energy levels are distinctly shifted by the topological defect parameter ($α$). The mass spectra of heavy quarkonia ($c\\bar{c}$ and $b\\bar{b}$) and fully-heavy tetraquarks ($cc\\bar{c}\\bar{c}$ and $bb\\bar{b}\\bar{b}$) across several radial and orbital excitation states are successfully calculated using this approach. The computed masses of bottomonium and charmonium accord well with current theoretical predictions and experimental findings. Our findings for the heavy tetraquarks are in line with previous theoretical investigations that consider tetraquarks as configurations of diquarks and antidiquarks. The numerical results demonstr","url":"http://arxiv.org/abs/2606.27363v1","contact":"","deadline":"2026-06-25T17:58:44Z","source":"arXiv","priority":5,"created_at":"2026-06-27T21:27:28.763349","quality_score":73,"quality_reason":"priority=5, has_url, trusted_source, good_description, detailed_description, good_tags"},{"id":1434,"type":"publication","title":"The Effect of Tour Guides' Communication Effectiveness on Tourists' Intercultural Interaction Levels","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,journal article","description":"Journal article. The primary aim of this study is to reveal the effect of tour guides' communication effectiveness on tourists' intercultural interaction levels, specifically within the context of incoming tours. In this regard, the study intended to analyze the effects of tour guides' communication effectiveness on intercultural interaction, the dependent variable, using scientific methods. The data collection tool used in the study was designed for both digital use via the Google Forms platform and for physical use. Accordingly, the data collection process was carried out in two formats: face-to-face interviews conducted by the researcher and Google Forms. In line with the research objective, data were collected from 263 participants using a survey. The analysis results revealed that tour guides' communication effectiveness positively influences tourists' intercultural interaction. Detailed analyses further confirmed a positive and significant effect on the sub-dimensions of intercultural interaction: emotional orientation, self-efficacy, and behavioral performance. Year 2 Final Report, USEPA Regional-ORD Applied Research (ROAR) Project #2554 This report presents the findings from the second year of the USEPA ROAR Project #2554, focused on adapting and extending the Flow Photo Explorer model to predict water levels in non-free flowing waterbodies, namely lakes and wetlands. The methodology through this project has been integrated into the USGS Flow Photo Explorer (FPE) platform (https://usgs.gov/apps/ecosheds/fpe), which is an integrated database, machine learning, and data visualization platform for monitoring streamflow and other hydrologic conditions using timelapse images. This report builds off the results from year 1 of the project, which can be found here: Walker, J. (2025). Low-cost Streamflow Monitoring using Timelapse Imagery and Machine Learning Models - Year 1 Report (Version v20250403). Zenodo. https://doi.org/10.5281/zenodo.15133342 Funding provided by USEPA ORD through the Regional-ORD Applied Research (ROAR) Project #2554. PCI Archaeo revision (round 1). This release accompanies the revised manuscript submitted to PCI Archaeology (#1019). It corrects the sign of the ICL model-selection criterion, adds two reviewer-requested refinements to the data-simulation and Harris-matrix helpers, and documents the model-selection metrics in both the help pages and the manuscript. The SEF model itself is unchanged since 0.17.1, so all case-study results reproduce identically.\n
\n
\n
This repository contains all relevant materials for the study, including:\n\n
AWS_environment.zip contains recordings of wind speed, wind direction and temperature at the Zhongshan Station from 6 Dec 2019 to 2 Jan 2020.
Rutford icestream data:
1. Rutford_ice_stream_das_data/icequakes_information.csv - A csv file containing icequake information, including origin times and seismic moment.
2. Rutford_ice_stream_das_data/tdms/*.tdms - Raw DAS data recordings over the time periods when the icequakes occured. Data is recorded by a Silixa iDas.
(All other information on the deployment can be found in Hudson et al. (2021), JGR).
3. Gornergletscher_das_data/gornerglethscer_das_qm_stations.csv - A file containing coordinates of all the fibre channels.
4. Gornergletscher_das_data/segy/*.sgy - Raw data files for the time periods used in this study.
by Folesky, Kummerow, Hofman, 2025
This file contains the repeating earthquake table, where events are grouped into repeater families, already.
cID : cluster ID
lat : event latitude or median of the sequence
lon : event longitude or median of the sequence
dep : event depth in km or median of the sequence
mag : magnitude or average magnitude for the sequence
stdmag: standard deviation of magnitudes in the sequence
numel : number of events in the sequence
td : total duration between first and last event in days
tr : average inter-event time
cvr : coefficient of variation
slip : slip in cm or cumulative slip in cm for the whole series, where each first event is neglected
sr : slip rate in cm/yr
tccls : tectonic location identifier similar to Muenchmeyer et. al, 2025
type : recurrence pattern type for sequences with n>3
coda_back_migration_movie.mov - A movie showing the back migration of the coda for one icequake through time.
gornerglethscer_das_and_nodes_qm_stations.csv - The locations of the DAS channels and nodal receivers.
gornergletscher_icequake_catalogue.csv - The entire filted icequake catalogue.
icequakes_selected_for_surface_wave_tomography.csv - The manually selected events used for the surface wave tomography.
source_inversion_data.zip - Data and results for the source inversion of 48 icequakes (including modelled and observed waveform data).
python_notebooks.zip - The python notebooks used for the surface wave tomography and automated icequake source mechanism inversions.
\nHudson, T. S., Kufner, S., Brisbourne, A. M., Kendall, J., Smith, A. M., Arthern, R., & Alley, R. (2023). Friction and slip measured at the bed of an Antarctic ice stream. Nature Geoscience.
\nall_icequakes_2018to2019.csv - A catalogue of the icequakes used in the study.
\ncluster_????.csv - csv files containing the results for each icequake, grouped by cluster (i.e. one csv file per cluster).
\nslip_rate_movie.mp4 - A movie of slip-rate for each icequake through time.
\n------------------------------------- all_icequakes_2018to2019.csv file -------------------------------------
\norigin_time - Origin time of icequake, in UTC time.
\nMw - Moment magnitude.
\nMw_err - Error in Mw.
\nfc - Corner frequency (Hz).
\nfc_err - Error in corner frequency.
\nQ - Quality factor (measure of attenuation).
\nQ_err - Error in Q.
\ninter-event_time_s - Inter-event time between this icequake and the previous icequake (s).
\nstress_drop - Stress-drop of icequake (Pa).
\nstress_drop_err - error in stress-drop.
\nlat - Latitude (decimal degrees).
\nlon - Longitude (decimal degrees).
\nx (km) - x grid location (km).
\ny (km) - y grid location (km).
\nz (km bsl) - Depth (km bsl).
\nx_err (km) - Error in x (km).
\ny_err (km) - Error in y (km).
\nz_err (km) - Error in z (km","url":"https://doi.org/10.5281/zenodo.7870307","contact":"Hudson, Thomas Samuel","deadline":"2023-04-27","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":1393,"type":"dataset","title":"Dataset for the manuscript \"Self-Supervised Coherence-Based Denoising of Cryoseismological Distributed Acoustic Sensing Data\"","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,dataset,cryoseismology,distributed acoustic sensing,denoising,Rhône Glacier,J-invariance","description":"Dataset.
This dataset provides the necessary data to reproduce the results presented in the paper “Self-Supervised Coherence-Based Denoising on Cryoseismological Distributed Acoustic Sensing Data.” The corresponding code is available on GitHub, and the paper can be accessed via Authorea.
The data sets , \"11_vanende_earth_denoisedDAS_image\", \"12_vanende_finetuned_cryo_denoisedDAS_image\", \"13_afk_denoisedDAS_image\", \"14_conventional_denoisedDAS_image\", and \"15_DASDL_denoisedDAS_image\" contain the some denoised data files for the models \"J-invariant-earth\", \"J-invariant-earth-cryo\", \"\"AFK\", \"Conventional\", and \"DASDL\" , needed for reproducing Figure 5, S7, and S8.
Abstract:
One major challenge in cryoseismology is that signals of interest are often buried within the high noise level emitted by a multitude of environmental processes. Events of interest potentially stay unnoticed and remain unanalyzed, particularly because conventional sensors cannot monitor an entire glacier. However, with Distributed Acoustic Sensing (DAS), we can observe seismicity over multiple kilometers. DAS systems turn common fiber-optic cables into seismic arrays that measure strain rate data, enabling researchers to acquire seismic data in hard-to-access areas with high spatial and temporal resolution. We deployed a DAS system on Rhonegletscher, Switzerland, using a 9 km long fiberoptic cable that covered the entire glacier, from its accumulation to its ablation zone, recording seismicity for one month. The highly active and dynamic cryospheric environ ment, in combination with poor coupling, resulted in DAS data characterized by a low Signal-to-Noise Ratio (SNR) compared to classical point sensors. Our objective is to ef fectively denoise this dataset.
We use a self-supervised J -invariant U","url":"https://doi.org/10.5281/zenodo.13890738","contact":"Zitt, Johanna","deadline":"2024-10-04","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":1459,"type":"dataset","title":"EAVES-KSA: elevation-area-volume curves for 526 Saudi Arabian reservoirs","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,dataset,reservoir,bathymetry,elevation-area-volume,SRTM,Saudi Arabia,arid hydrology,water storage,dams","description":"Dataset. \n
\n
\nStevens, N.T., Zoet, L.K., Hansen, D.D., Alley, R.B., Roland, C.J., Schwans, E., and Shepherd, C.S. (In Review) Icequake insights on transient glacier slip mechanics near channelized subglacial drainage. Earth Planet. Sci. Lett.
\n
mb_ctl.csv: Results with the precipitation parameter (r_P=1.48)
mb_ngt.csv: Results with the lower bound of precipitation parameter (r_P=1.40)
mb_pst.csv: Results with the upper bound of precipitation parameter (r_P=1.56)
mb_nc.csv: Results without calibrating precipitation parameter (r_P=1.00)
year: Year
B: Glacier-wide mass balance (mm w.e.)
P: Precipitation (mm w.e.)
Psnow: Snow (mm w.e.)
Prain: Rain (mm w.e.)
Tsum: Summer mean air temperature (degC)
PDD: Positive degree day (degC day)
d_melt: Day of melting (day)
Tequi: Summer mean temperature to yield zero-mass balance (degC)
Water Resources Research manuscript on engineering superposition and water-quality
risk in the middle–lower Han River (South-to-North Water Diversion donor reach).
Layer 1 — Multivariate autoencoder anomaly detection
Layer 2 — Spatial difference-in-differences and simplified CausalImpact
Layer 3 — Convergent cross-mapping (CCM)
Layer 4 — Hydrological closure tests (A1: flow–dilution; A2: engineering groups;
A3: impoundment signal)
environment.yml for dependency installation.
• 10-station monthly water-quality time series (confidential)
• Main-station monthly discharge archive (confidential)
identifiers). Qualified researchers may request raw data from the data providers
listed in the manuscript Open Research section.Replication Package – Code Smells in Clojure: Initial Findings from a Grey Literature Review
\n\n
\nCode_Smells_in_Clojure__Early_Results_from_a_Grey_Literature_Review.pdf included in this repository.Abstract
\n
This file shows a 3d view of the glacier surface of 2023 and the interpolated bedrock (Ordinary Kriging) from the July 2025 recordings. The observed features of the three surveys (April 2025, July 2025, March 2026) are on display.
In folder ASCII, there are the files DAT_0116_A1, DAT_0117_A1, DAT_0120_A1, DAT_0125_A1, DAT_0126_A1, DAT_0129_A1, DAT_0130_A1 which are the GPR acquisition lines recorded on Hintereisferner. They are readable in ReflexW (sandmeier-geo.de), can be processed with provided Sequence Processing Flow. In LINEDATA, the picked bedrock and features can be found to be opened in ReflexW.
In folder ASCII, there are the files DAT_0146_A1, DAT_0147_A1, DAT_0148_A1, DAT_0149_A1, DAT_0150_A, which are the GPR acquisition lines recorded on Hintereisferner. They are readable in ReflexW, can be processed with provided Sequence Processing Flow. In LINEDATA, the picked bedrock and features can be found to be opened in ReflexW.
This dataset is acquired with another radarsystem than April and July 2025 and therefore provided in folder PROCDATA. There are the files LINE__4.03 (without GPS coordinates), LINE__6.04 with coordinates in folder ASCII, LINE__08.04 (without coordinates). Readable in ReflexW, can be processed with provided Sequence Pro","url":"https://doi.org/10.5281/zenodo.20815613","contact":"Walker, Céline, Jovanovic, Nikola, Koch, Moritz, Felix Pfluger, Prinz, Rainer, Cook, Samuel","deadline":"2026-06-23","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":1274,"type":"publication","title":"Debonding mechanism analysis of ice-rock interface using frequency domain generalized multi-symplectic method","institution":"Applied Mathematical Modelling","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":"Crossref publication metadata. Journal: Applied Mathematical Modelling. Authors: Zhengqi Han, Weipeng Hu, Xinying Yan, Chuan Xiao, Chuanzeng Zhang, Zichen Deng. Year: 2027.","url":"https://doi.org/10.1016/j.apm.2026.117127","contact":"Zhengqi Han, Weipeng Hu, Xinying Yan, Chuan Xiao, Chuanzeng Zhang, Zichen Deng","deadline":"2027","source":"Crossref","priority":6,"created_at":"2026-06-27T21:51:40.076393","quality_score":0,"quality_reason":""},{"id":1245,"type":"publication","title":"Decoupled lake-glacier hydrological responses to Holocene climate forcing on the central Tibetan Plateau","institution":"CATENA","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":"Crossref publication metadata. Journal: CATENA. Authors: Qiangqiang Kou, Liping Zhu, Teng Xu, Qingfeng Ma, Xiangjun Wu, Junbo Wang, Jianting Ju, Thorsten Bauersachs. Year: 2026.","url":"https://doi.org/10.1016/j.catena.2026.110263","contact":"Qiangqiang Kou, Liping Zhu, Teng Xu, Qingfeng Ma, Xiangjun Wu, Junbo Wang, Jianting Ju, Thorsten Bauersachs","deadline":"2026","source":"Crossref","priority":6,"created_at":"2026-06-27T21:51:40.076393","quality_score":0,"quality_reason":""},{"id":1026,"type":"publication","title":"Deep-water hydrographic variability in the Northeast Atlantic during MIS 4","institution":"University of Cambridge, University College London","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,stadial,hydrography,oceanography,geology,marine isotope stage,glacial period","description":"Abstract. Understanding the evolution of deep ocean circulation and chemistry over the last glacial cycle is key for elucidating the ocean’s role in modulating atmospheric CO2 changes on millennial and orbital timescales. Marine Isotope Stage (MIS) 4 is a key paleoclimatic interval of the last glacial inception for assessing the role of the deep-ocean carbon storage in driving atmospheric CO2 levels, because it is characterized by a large decrease of air temperature and a rapid atmospheric CO2 drop of ~40 ppmv, likely linked to changes in ocean circulation, and includes several millennial climatic events, for example Heinrich Stadial (HS) 6. Although previous proxy-based studies have suggested a weakened Atlantic overturning during MIS 4, and particularly HS 6, basin wide changes in circulation remain poorly constrained. Here, we present high-resolution deep-water hydrography reconstructions from the mid-depth Iberian Margin (core MD01-2444, ~2.65 km water depth), based on benthic foraminiferal Mg/Ca-derived deep-water temperature (Tdw), benthic δ18O, and associated δ18Odw records, alongside SS- based flow-speed record. Our data reveal three distinct deep-water hydrographic ‘regimes’ at the Iberian Margin: 1) warm “interglacial-like” mode during MIS 5a (including Greenland stadials C19 and C20); 2) a colder glacial circulation mode during early MIS 4 (pre- HS 6); and 3) a “Heinrich” circulation mode during HS 6. A stronger influence of colder southern-sourced waters is inferr","url":"https://doi.org/10.5194/egusphere-2026-3334","contact":"Svetlana Radionovskaya, Mervyn Greaves, David Thornalley, Luke C. Skinner","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":613,"type":"publication","title":"Design of a Maritime-Themed Toy for Preschool Children","institution":"Sapienza University of Rome","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,brainstorming,subconscious,cognition,psychology,early childhood,engineering","description":"This paper focuses on early childhood education aimed at promoting maritime military culture and science education. It proposes the design of an educational board game based on a maritime military theme, intended to provide children with foundational learning. Through the introduction and popularisation of knowledge regarding ships and maritime navigation, children can develop an understanding of China’s naval affairs from an early age. At the same time, parents remain keenly interested in experiential, interactive education for their children. Many parents face challenges in selecting early learning toys and are increasingly prioritising the importance of subconscious education and companion-based parent-child interaction during their children’s development. This project is aimed at pre-school children aged 3–6. Based on the fundamental principles of convenience, safety and ease of use in children’s toys, it integrates learning through play into daily life. During play, it cultivates children’s spatial awareness of shapes and expands their logical thinking. By gradually increasing the game’s difficulty, it encourages brainstorming and stimulates visual senses, thereby sparking creativity, achieving cognitive balance and enhancing cognitive abilities.","url":"https://doi.org/10.63593/as.2709-9830.2026.03.003","contact":"Chen Chengcheng","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":339,"type":"publication","title":"Detecting Tidal Resonances in Binary Neutron Stars","institution":"arXiv","country":"International","city":"","latitude":null,"longitude":null,"tags":"arxiv,publication,preprint","description":"As a binary neutron star inspirals due to the emission of gravitational waves, the rising tidal frequency resonantly excites vibrational modes. These oscillations are seismological probes of the rich stellar interior, yet it remains to be established whether gravitational-wave interferometers can measure them. Here, we present the first fully Bayesian study of the capability of the Einstein Telescope to detect tidal resonances. We simulate one year of observations and analyse the 200 loudest signals. We find that the Einstein Telescope can identify resonant modes and is sensitive to gravitational-wave phase shifts as small as $ΔΦ\\approx 0.03$ for favourable events. We further show that neglecting resonances can bias the inferred tidal deformabilities. These results establish tidal resonances as a measurable route for asteroseismology with future detectors.","url":"http://arxiv.org/abs/2606.06376v1","contact":"","deadline":"2026-06-04T16:45:17Z","source":"arXiv","priority":5,"created_at":"2026-06-27T21:27:28.763349","quality_score":73,"quality_reason":"priority=5, has_url, trusted_source, good_description, detailed_description, good_tags"},{"id":452,"type":"publication","title":"Detection of glacier calving events from time-lapse images using computer vision and a neural network","institution":"University of York, Polish Academy of Sciences, AGH University of Krakow","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,ice calving,artificial intelligence,glacier,artificial neural network,geology,computer vision","description":"Abstract Ground-based time-lapse cameras are often used to monitor glacier recession, which is primarily driven by the falling of ice from the glacier front, known as iceberg calving or, more commonly, calving events. Glaciologists can utilise these images by manually identifying calving events, a laborious task that requires the analysis of thousands of images in order to identify image pairs that represent the glacier front before, during and after calving. We present a computer vision based method to filter out images rendered unusable due to weather effects such as fog and precipitation by calculating the number of salient key-points detected in the image using the SIFT (Scale-Invariant Feature Transform) algorithm as an indicator of the visibility of the glacier front and discarding any image with fewer key-points than a defined threshold. We propose the use of SNN (Siamese neural network) and show that it is useful in detecting calving events since it allows to separately calculate features on two images and then merges them together in order to track differences between them thus detecting calving areas. The trained model achieved an overall accuracy of 92%, with 79% of calving events and 93% of non-calving being correctly classified on an unseen test set formed from imagery in the same time period as the training data. The model was able to generalise to new time periods (and therefore small changes in viewpoint and alignment) to some extent with an overall accuracy o","url":"https://doi.org/10.1017/jog.2025.10115","contact":"Lakhan Mankani, Oskar Glowacki, William A. P. Smith, Paulina Lewińska","deadline":"2025","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":893,"type":"publication","title":"Determination of Waste Thickness of the Closed Solid Waste Site, Halkalı, Istanbul, Türkiye","institution":"Istanbul University, Istanbul University-Cerrahpaşa","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,leachate,environmental science,context (archaeology),rainwater harvesting,municipal solid waste,groundwater","description":"The aim of this study is to analyze the closed Halkalı solid waste landfill in Istanbul using Ground Penetrating Radar (GPR) in order to evaluate the depth and spatial distribution of accumulated waste. The landfill, which operated between 1983 and 1994, has raised concerns regarding its future usability due to potential environmental risks. The research focuses on Menekşe Valley, located between the Menekşe and Hasanoğlu streams, and aims to determine whether the remaining waste thickness at the site poses a potential contamination threat, particularly in the context of increasing urban development interest. GPR surveys conducted with 38 MHz and 75 MHz antennas revealed waste layers at depths ranging from 5 to 15 meters, indicating significant heterogeneity within the study area. These findings may suggest a potential environmental risk associated with leachate generation due to rainwater infiltration; however, a more reliable assessment would require detailed characterization of the leachate and/or systematic monitoring of groundwater quality. The results of this study are of great importance for assessing the site’s suitability for development, shaping environmental policies, and providing scientific data to support land-use planning.","url":"https://doi.org/10.54365/adyumbd.1807473","contact":"Fethi Ahmet Yüksel, Nihan Hoşkan","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":402,"type":"publication","title":"Deterministic statistical patterns preceding ice shocks revealed by ice deformation measurements","institution":"Crimean Astrophysical Observatory, Institute of the Earth’s Crust","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,geology,deformation (meteorology),statistical analysis,geodesy,deformation monitoring,geophysics","description":"Ice shocks associated with the springtime thermal expansion of ice represent a manifestation of fracture processes in a complex nonlinear medium. In this study, we investigate temporal changes in statistical characteristics derived from ice deformation measurements preceding such events. The analysis demonstrates that the approach of ice shocks is accompanied by the formation of ordered linear features that constrain the evolution of a statistical functional constructed from deformation data. These features indicate a transition from predominantly stochastic behavior to the emergence of deterministic patterns in the system dynamics. A detailed examination of the temporal evolution of the statistical dependencies reveals several distinct groups of short-term precursors. The earliest indicators appear approximately one hour before an ice shock, followed by a second group emerging on the order of tens of minutes prior to the event. A further concentration of precursor signatures is observed within the final minutes preceding ice failure. Particular attention is given to the increasing topological similarity of the statistical patterns observed during these intervals, suggesting a progressive synchronization of deformation processes prior to fracture. The results support the applicability of statistical and topological analysis for identifying short-term precursors of ice shocks and highlight the potential of this approach for studying explosive-like processes in other complex na","url":"https://doi.org/10.1038/s41598-026-44091-6","contact":"A. E. Volvach, S. A. Bornyakov, L. P. Kogan, L. N. Volvach","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":390,"type":"publication","title":"Deterministic structures in functionals of Baikal ice deformations","institution":"Crimean Astrophysical Observatory, Institute of the Earth’s Crust","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,geology,deformation (meteorology),geometry,field (mathematics),physics,geophysics","description":"This study investigates deterministic structures in statistical functionals derived from high-resolution measurements of Lake Baikal ice cover deformations preceding ice shocks - events caused by thermal expansion during spring warming. Understanding these precursors is essential for reliable forecasting in cryoseismology. Using statistical-functional analysis, the measured signals are decomposed into background noise and precursor-related components. Deterministic linear structures of the function, including channels and sliding boundaries, as well as short-term precursors lasting up to one hour, are identified. Spatially distributed measurements show high topological similarity of the statistical functionals preceding ice shocks. These findings demonstrate the effectiveness of nonlinear functional analysis in detecting early-warning signals and provide a framework for future studies on natural hazard prediction.","url":"https://doi.org/10.1080/19475705.2026.2669026","contact":"A E Volvach, S.A. Bornyakov, L. P. Kogan, L. N. Volvach","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1168,"type":"publication","title":"Dietary niches of three resident phocid seal species in Kongsfjorden, Svalbard, Norway","institution":"OpenAlex","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,phoca,biology,arctic,benthic zone,pelagic zone,harbor seal","description":"Abstract Arctic marine ecosystems are undergoing borealization due to global warming. In the Svalbard Archipelago (Norway), this has resulted in the harbor seal ( Phoca vitulina vitulina ) expanding its distribution along the west coast, such that this species now coexists sympatrically with Arctic endemic ringed seals ( Pusa hispida hispida ) and bearded seals ( Erignathus barbatus barbatus ) in several fjords. This study investigated feeding strategies and niche overlaps among the three seal species resident in Kongsfjorden using stable isotope (SI) ratios in skin and fatty acid (FA) profiles in blubber, along with both tracers in potential prey, sampled 2021–2023. Ringed seals exhibited significantly lower δ¹³C values (-25.5 ± 1.7‰) compared to harbor (-22.1 ± 3‰) and bearded seals (-20.8 ± 3.2‰), reflecting their pelagic feeding habits, while harbor and bearded seals consumed more benthic prey. Large variation in δ 15 N and δ 34 S in ringed seals suggests that some individuals get nutrients from freshwater/terrestrial sources, which is likely related to their feeding near tidewater glacier fronts. Principal component analyses of FA profiles revealed that ringed seals consumed FAs from haptophytes/dinoflagellates (18:4n3), whereas harbor and bearded seals had FAs from protozoan/macroalgae (20:4n6) and copepod (20:1n11) sources. Bearded seals had the highest FA-niche overlap with harbor seals (92.1%), suggesting foraging similarities in shallow, near-shore habitats. Ringed ","url":"https://doi.org/10.1007/s00300-026-03507-9","contact":"Olof Bengtsson, Christian Lydersen, Aaron T. Fisk, Jan Marcin Węsławski, Jørgen Berge, Kit M. Kovacs","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1052,"type":"publication","title":"Diffuse Adiabatic Flows in Thermally Coupled Grounded Shallow Ice Sheets: Modelling and Analysis","institution":"OpenAlex","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,adiabatic process,ice sheet,geology,mechanics,grounded theory,surface (topology)","description":"In this article we propose a novel thermodynamical model which couples the evolution of the thickness of a grounded shallow ice sheet with the evolution of its internal temperature. Both the grounded shallow ice sheet surface elevation and the ice internal temperature are subjected to physical constraints. The equations governing the evolution of the grounded shallow ice sheet thickness are degenerate, and the ice internal temperature evolves in a moving domain. First, we formally model the phenomenon under consideration by adopting strategies akin to those employed in the construction of diffuse-interface models. Second, we establish the existence of solutions for one such formal model by means of the penalty method, and we observe that the low regularity of the problem under consideration prevents us from obtaining a standard concept of solution.","url":"https://openalex.org/W7164973266","contact":"Paolo Piersanti","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1156,"type":"publication","title":"Dimethylsulfoniopropionate metabolism shapes microbial ecology and physiological adaptation during the austral winter in Southern Ocean sea ice and seawater","institution":"Stellenbosch University, University of Pretoria, European Bioinformatics Institute, Wellcome Trust, Stazione Zoologica Anton Dohrn, University of East Anglia, Norwich Research Park, Quadram Institute","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,dimethylsulfoniopropionate,sea ice,algae,seawater,sulfur cycle,ecology","description":"Dimethylsulfoniopropionate (DMSP) is a highly abundant marine organosulfur compound, with important roles in stress protection and climate-cooling gases production. Polar regions, particularly seawater and sea ice interfaces, are critical yet understudied DMSP cycling hotspots. Here, we reveal up to 38-fold higher DMSP concentrations in Southern Ocean sea ice versus seawaters, identifying sea ice as a concentrated reservoir of DMSP with implications for microbial stress tolerance and sulfur recycling. Eukaryotic algae harboring DSYB and DSYE genes were predicted to dominate DMSP production, but diverse and previously unidentified bacterial producers were also detected. This elevated abundance of algal biosynthetic genes likely underpins the higher DMSP concentrations in sea ice. Notably, DMSP catabolism, particularly the dmdA demethylase and dddD and dddK lyase genes, were more abundant than biosynthesis genes. Taken together, these findings reveal the widespread metabolism for DMSP cycling and underscore a dynamic reservoir and transformation hub influencing polar climate-cooling sulfur fluxes.","url":"https://doi.org/10.1038/s41467-026-73596-x","contact":"Z. Mayibongwe Buthelezi, Rian Pierneef, Oliver K. I. Bezuidt, M. Nello J. Gregori, Stéphane Pesant, Daniele Iudicone, Libby Hanwell, Jonathan D. Todd","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":591,"type":"publication","title":"Diversity and Community Structure of Bacteria in High-Altitude Proglacial Lakes in Southern Qinghai-Xizang Plateau","institution":"Plateau State University","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,community structure,species richness,ecology,habitat,environmental science,plateau (mathematics)","description":"The proglacial lakes of the Qinghai-Xizang Plateau serve as natural laboratories for studying microbial adaptation to extreme environments. However, research on the composition and functional characteristics of microorganisms in these settings remains limited. In this study, three typical high-altitude proglacial lakes in southern Xizang (Qudengnima proglacial lake, Gangbugou proglacial lake, and Qiangyong proglacial lake) were selected as research subjects. Bacterial community structure, diversity in the water and sediment of these lakes were analyzed using 16S rRNA sequencing. The results showed that Pseudomonadota, Actinomycetota, and Bacteroidota were highly abundant across all samples. The relative abundances of Cyanobacteriota and Acidobacteriota, however, exhibited distinct habitat preferences: Cyanobacteriota was enriched in the water, whereas Acidobacteriota was predominantly found in sediment. Alpha diversity analysis showed that both species diversity and richness in Qiangyong proglacial lake were significantly higher than those in the other proglacial lakes, and within the same lake, both diversity and richness in sediment were higher than in the water. Beta diversity analysis indicated that the bacterial community structures in sediment were similar across different proglacial lakes, whereas those in water varied considerably among the lakes. LEfSe analysis identified 94 biomarkers that exhibited significant differences among the different proglacial lake environ","url":"https://doi.org/10.3390/microorganisms14071398","contact":"Yapeng Zheng, Dorji Phurbu","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":341,"type":"publication","title":"DnA: Denoising Attention for Visual Tasks","institution":"arXiv","country":"International","city":"","latitude":null,"longitude":null,"tags":"arxiv,publication,preprint","description":"The softmax activation in multihead attention (MHA) is the de facto standard for attention-based models in visual perception tasks. However, standard softmax can produce noisy attention patterns that dilute relevant features and degrade its performance. In this paper, we propose Denoising Attention or DnA, in which, first, a positive query identifies which image features belong to the correct class, and a negative query identifies closely associated but irrelevant image features. DnA then projects these interactions into two distinct subspaces with larger principal angles, promoting subspace separation and improved discriminability. Using a ViT-B backbone, our proposed DnA achieves an absolute gain of 0.8% on ImageNet-1K compared to the baseline. We further show improvements across multiple visual understanding tasks, including video understanding with video transformers (1.8%) and video LLMs (0.5%). Our extensive empirical analyses justify the design choices involving two interacting subspaces and the denoising effect of DnA.","url":"http://arxiv.org/abs/2606.27372v1","contact":"","deadline":"2026-06-25T17:59:48Z","source":"arXiv","priority":5,"created_at":"2026-06-27T21:27:28.763349","quality_score":73,"quality_reason":"priority=5, has_url, trusted_source, good_description, detailed_description, good_tags"},{"id":767,"type":"publication","title":"Downscaling Daily Discharge to Sub‐Daily Scales for Alpine Glacierized Catchments","institution":"Centre National de la Recherche Scientifique, Université de Bordeaux, Free University of Bozen-Bolzano, University of Lausanne, Oeschger Centre for Climate Change Research, FORS – Swiss Centre of Expertise in the Social Sciences, University of Padua","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,downscaling,environmental science,climatology,meteorology,scale (ratio),climate change","description":"Abstract Hydrological dynamics in glacierized catchments of the Alps are shaped by temperature‐driven processes, including snow and ice melt as well as precipitation, leading to diel streamflow cycles that vary in intensity within‐ and among‐the seasons. During the summer melt period, the amplitude of these diel cycles increases due to diminished snow storage and the emergence of efficient subglacial drainage systems. Accurately modeling these sub‐daily cycles remains difficult, due to a lack of high‐resolution meteorological input data for melt simulations and due to challenges in parameterizing meltwater routing through dynamic glacial systems. This research develops an approach for downscaling daily streamflow timeseries to sub‐daily timescales (daily flow duration curves) in alpine glacierized catchments influenced by snow and ice melt runoff. We adapt a maximum entropy framework (POME) to the specificities of glacial systems, that we calibrate on a 45‐year data set of 15‐min discharge records from seven glacier‐fed catchments in the southwestern Swiss Alps. The calibrated method is then applied to the outputs of a semi‐lumped hydrological model that simulates daily discharge and provides hydrological variables such as snow depth and ice melt to inform the downscaling, and the results are evaluated against observed discharge. Our results reveal that a sigmoid function effectively represents seasonally varying daily flow duration curves in glacierized catchments and highli","url":"https://doi.org/10.1029/2025wr040699","contact":"A.-L. Argentin, M. Gianini, B. Schaefli, P. Horton, V. Chavez-Demoulin, F. Pitscheider, L. Repnik, S. Bizzi","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1034,"type":"publication","title":"Dust Record from Allan Hills Blue Ice: Towards Extending the Archive to 4000 ka","institution":"University of Wisconsin–Madison, Scripps Institution of Oceanography, Princeton University, University of California San Diego, Oregon State University, Woods Hole Oceanographic Institution, University of Washington, Earth and Space Research, Dartmouth College","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,geology,ice core,glacial period,interglacial,loess,weathering","description":"Abstract. Previous analyses of dust concentration and size distribution in ice cores are limited to the past 800,000 years; however, the ALHIC1901 ice core drilled at the Allan Hills Blue Ice Area (BIA) in East Antarctica provides a unique opportunity to examine older discontinuous records of ice ranging in age from 4000–500 ka. Here we present a discrete record of insoluble particles within ALHIC1901 from the bottom 25 m of the core. We investigated the particle mass concentration, size distribution, and mineralogy within the core to assess the preservation of dust records in BIAs with complex flow histories. We find that the insoluble particle concentrations are likely altered by entrainment of basal sediment for depths 5 m above bedrock. For shallower depths less affected by subglacial input, the record lacks expected peaks in dust concentration during glacial periods, which have been termed “long snapshots,” implying that low net accumulation rates during glacial periods at the Allan Hills BIA results in the preferential loss or attenuation of glacial ice and a corresponding bias toward the preservation of interglacial ice. The dust concentrations may also be further smoothed due to ice thinning. A subset of particles from both the upper and lower ranges of depths analyzed shows evidence of mineral weathering and/or in situ production of secondary minerals, and insoluble particle concentration correlates well with non-atmospherically derived carbon dioxide concentrations.","url":"https://doi.org/10.5194/egusphere-2026-2434","contact":"Alissa Choi, A. Carter, Julia Marks-Peterson, Sarah Shackleton, John A. Higgins, Edward J. Brook, Liam Kirkpatrick, Jacob I. Chalif","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":676,"type":"publication","title":"EARLY PLIOCENE DRAWDOWN AND EXPANSION OF THE ANTARCTIC PENINSULA ICE SHEET IN MARGUERITE BAY","institution":"OpenAlex","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,geology,ice sheet,oceanography,glacial period,antarctic ice sheet,ice stream","description":"The Antarctic Peninsula Ice Sheet (APIS) is situated in a rapidly and persistently warming region of Antarctica and its behavior under warmer conditions projected for Earth’s future remains poorly constrained. Interpretations of stratigraphic records of ice-sheet change from periods of warmth in Earth’s past are essential in providing boundary conditions for estimates of future ice loss and its climate feedbacks. The early Pliocene exhibited surface temperatures that were 3-4 °C higher than present under similar greenhouse forcing. Here we present new sedimentological and geochemical data from the early Pliocene section recovered in Ocean Drilling Program Site 1097 to assess the effects of atmospheric and ocean warming on ice extent and glacial regime. The reconstruction of Pliocene glacial processes and sediment provenance within an updated chronology of Site 1097, indicates that ice was absent from the Marguerite Bay with supply from local glaciers only at ~5.2 to 4.8 Ma. A subsequent shift in sediment provenance suggests that the APIS began to dominate ice drainage into Marguerite Bay ~4.5 Ma with the sedimentology of the deposits pointing to a subpolar, meltwater-intensive glacial system before ~4.3 Ma. In contrast, a massive and stratified diamictite-dominated section younger than ~4.3 Ma, shows characteristics similar to Pleistocene deposits from the Marguerite Ice Stream Trough. These changes in sedimentary systems reflect enhanced accumulation and retreat phases of th","url":"https://doi.org/10.31223/x5bf5w","contact":"Sandra Passchier, Ridley Joseph, Monika Ghimire, Xiaona Li","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1458,"type":"publication","title":"EAVES: Elevation-Area-Volume Estimation from SRTM","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,software,hydrology,reservoir,bathymetry,elevation-area-volume,SRTM,arid basins,dams","description":"Software.
outcomes, considering various channels through which gender,
growth, and development interact. It upholds the salience not only of equality
in opportunities but also equality in outcomes. The contribution argues that
inequalities based on gender, race, ethnicity, and class undermine the ability to
provision and expand capabilities, and it examines the macroeconomic policies
that are likely to promote broadly shared development. It explores how the
macroeconomy acts as a structure of constraint in achieving gender equality and
in turn how gender relations in areas like education and wage gaps can have
macro-level impacts. Further, it underscores that the interaction of the
macroeconomy and gender relations depends on the structure of the economy,
the nature of job segregation, the particular measure of gender inequality, and
a country’s international relations. Finally, it outlines policies for promoting
gender equality as both an intrinsic goal and a step toward improving
well-being.
2. data/raw/positives/ — positive interaction records curated from six public databases (IntAct, BioGRID, HPIDB, PHISTO, VirHostNet, PHILM2WEB)
3. data/raw/negatives — negative samples generated by the authors
4. data/processed/ — processed protein sequence feature vectors
5. results/ — benchmark outputs
6. requirements.txt (the required libraries for running the pipeline)Changed
\n\n
","url":"https://doi.org/10.5281/zenodo.20945859","contact":"Kristenson, Heidi, Smale, Jacquelyn, Johnston, Andrew, Herrmann, Jake, Gens, Rudi, Kennedy, Joseph H, White, Julia, Lewandowski, Alex","deadline":"2026-06-27","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":901,"type":"publication","title":"Neanderthals in dynamic Landscapes: Climate variability and human occupation from MIS 5-3 at Axlor cave (Northern Atlantic Iberia)","institution":"Universidad de Cantabria, Instituto de Física de Cantabria, Institute of History, Centre National de la Recherche Scientifique, Université de Bordeaux","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,cave,geography,geology,climate change,archaeology,paleontology","description":"We present palynological evidence and associated environmental and adaptive inferences from a long sequence of Neanderthal occupations robustly dated between MIS 5 and MIS 3 at Axlor. The cave lies in the southwesternmost sector of the Eurosiberian biogeographic region, in northern Atlantic Iberia. This coastal strip acted as a refugium for temperate taxa under adverse Upper Pleistocene climates, with persistent representation of mixed deciduous forest taxa. Quercus , Corylus , Castanea , Fagus , Taxus , Juglans , Crataegus and Prunus are recorded across nine stadial and interstadial phases. Riparian taxa, including Alnus , Fraxinus and Salix , are well represented, indicating permanent watercourses during most phases. Despite the resilience of temperate forests, marked shifts in landscape structure occurred, modulated by climatic fluctuations. In our record these changes are expressed primarily in forest cover, forest composition and grassland extent. Nonetheless, the region consistently provided a stable niche of exploitable resources for Neanderthal groups between ca. 107 - 42 ka BP. Axlor thus offers strong evidence for Neanderthal adaptive capacity in both forested (interstadial) and cold, open (stadial) settings. The robustness of the chronological framework and the richness of the pollen dataset make Axlor a key site for understanding the landscapes inhabited by Neanderthals during the Last Glacial Cycle along the southern margin of the Eurosiberian region.","url":"https://doi.org/10.1016/j.quascirev.2026.110098","contact":"Sebastián Pérez Díaz, Jesús Emilio González Urquijo, José Antonio López Sáez, Talía Lazuén Fernández","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":262,"type":"publication","title":"Near-Surface Characterization Using Integrated MASW and Seismic Refraction Tomography: A Scoping Review","institution":"University of Mataram","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,geology,seismic refraction,bedrock,borehole,seismology,characterization (materials science)","description":"Subsurface characterization is essential in engineering geology, geotechnical engineering, hydrogeology, and disaster mitigation because subsurface material conditions influence soil stability, seismic response, weak-zone identification, and infrastructure suitability. This study aims to map the development, characteristics, advantages, limitations, and research gaps related to the use of Multichannel Analysis of Surface Waves (MASW) and Seismic Refraction Tomography (SRT) in subsurface analysis. A scoping review approach was employed following PRISMA-ScR guidelines. Literature was obtained from ProQuest, ScienceDirect, and SpringerLink for the 2012–2026 publication period. Of the 852 articles identified, 23 studies met the inclusion criteria and were analyzed further. The findings show that MASW is effective for identifying variations in shear wave velocity (Vs), Vs30, soft layers, soil stiffness, and dynamic site response, whereas SRT is more effective for mapping compression wave velocity (Vp), layer thickness, bedrock boundaries, and lithological contrasts. The integration of MASW and SRT provides more robust subsurface interpretation, particularly in landslide, karst, landfill, sabkha, hydrogeological, and post-earthquake areas. However, several important research gaps remain, including the lack of standardized integration protocols, limited investigation depth, minimal validation with borehole data, ambiguity in integration with Horizontal-to-Vertical Spectral Ratio met","url":"https://doi.org/10.58578/mikailalsys.v4i2.10504","contact":"Syamsuddin Syamsuddin, Kormil Saputra, Olfi Destika, Winny Anindya Nadi, Zaura Intan Zaraoda","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:18:32.932503","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":428,"type":"publication","title":"Near-surface liquid water on Mars inferred from seasonal marsquakes","institution":"Peking University, Northwest University, University of Hong Kong, Chinese Academy of Sciences, Institute of Geology and Geophysics, University of Chinese Academy of Sciences, Southern University of Science and Technology, Center for High Pressure Science and Technology Advanced Research, Center for ","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,martian,mars exploration program,geology,water cycle,liquid water,groundwater","description":"Exploring the presence and behavior of water on Mars is critical for understanding the planet’s geological evolution, hydrological processes, and potential habitability, which has been a central objective of past and ongoing Martian exploration missions. Martian geomorphology provides evidence of ancient groundwater activity, but confirmation of present-day liquid water remains limited. Here, we infer near-surface brines confined to meter-scale depths in regions north of about 30 °N in the northern hemisphere, based on the analysis of seasonal variations in marsquake seismicity and thermal modeling. The absence of seasonal marsquakes during colder periods and their abrupt resurgence in warmer seasons can be explained by ice-to-brine phase transitions. Our findings reveal a mechanism whereby seasonal melting of subsurface ice elevates pore pressure and lubricates faults, leading to a reduction in frictional strength, and ultimately inducing marsquakes. This mechanism accounts for the seasonal variation, clustering, high seismic b-values, and shallow focal depths of seasonal marsquakes. Additionally, we estimate that the melting point of briny ice on Mars is below approximately 250 ± 13 K, advancing our understanding of Mars’ present-day brine cycle and near-surface hydrological processes. The study finds that seasonal marsquake patterns may indicate active near-surface brines on Mars today. By connecting seismicity changes to ice-to-brine melting, it infers that shallow liquid","url":"https://doi.org/10.1038/s41467-025-67784-4","contact":"Jing Shi, Jiaqi Li, Caoanla Li, Haoran Meng, Cong Sun, Chao Qi, Lu Pan, Siteng Fan","deadline":"2025","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1256,"type":"publication","title":"Near-threshold fatigue crack propagation in a CoCrFeMnNi high-entropy alloy: The role of microstructural state and crack-boundary interaction","institution":"Journal of Materials Science & Technology","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":"Crossref publication metadata. Journal: Journal of Materials Science & Technology. Authors: Yunji Park, Sangeun Park, Hyokyung Sung. Year: 2027.","url":"https://doi.org/10.1016/j.jmst.2026.05.003","contact":"Yunji Park, Sangeun Park, Hyokyung Sung","deadline":"2027","source":"Crossref","priority":6,"created_at":"2026-06-27T21:51:40.076393","quality_score":0,"quality_reason":""},{"id":575,"type":"publication","title":"Nested operator inference for adaptive data-driven learning of reduced-order models","institution":"The University of Texas at Austin","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,parameterized complexity,computer science,inference,algorithm,snapshot (computer storage),theoretical computer science","description":"This paper presents a data-driven, nested Operator Inference (OpInf) approach for learning physics-informed reduced-order models (ROMs) from snapshot data of high-dimensional dynamical systems. The approach exploits the inherent hierarchy within the reduced space to iteratively construct initial guesses for the OpInf learning problem that prioritize the interactions of the dominant modes. The initial guess computed for any target reduced dimension corresponds to a ROM with provably smaller or equal snapshot reconstruction error than with standard OpInf. Moreover, our nested OpInf algorithm can be warm-started from previously learned models, enabling versatile application scenarios involving dynamic basis and model form updates. We demonstrate the performance of our algorithm on a cubic heat conduction problem, with nested OpInf achieving a four times smaller error than standard OpInf at a comparable offline time. Further, we apply nested OpInf to a large-scale, parameterized model of the Greenland ice sheet where, despite model form approximation errors, it learns a ROM with, on average, 3 % error and computational speed-up factor above 19,000.","url":"https://doi.org/10.1007/s10444-026-10322-7","contact":"Nicole Aretz, Karen Willcox","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":811,"type":"publication","title":"Next-generation radar bed measurements should be optimized for assimilation or repeat-pass profiling","institution":"Stanford University, Sandia National Laboratories, Georgia Institute of Technology, Cornell University, University of Florida, Florida College","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,depth sounding,radar,geology,data assimilation,remote sensing,echo sounding","description":"Ice-penetrating radar observation of bed echoes is a core geophysical technique in glaciology. In early and ongoing exploration and mapping surveys, areas with little or no data were often prioritized, leading to few repeated radar sounding profiles. In parallel, advances in radar sounding instruments, platforms and analysis approaches have dramatically opened possibilities for future survey design. Here, we consider the opportunities these advances present for next-generation bed measurements, including both assimilation-optimized mapping and repeat sounding. Based on this analysis, we argue that repeat-pass profiles of bed echo power and englacial layer echo phase should be key priorities for future observations. To that end, we evaluate the detectability of subglacial water bodies, including ocean intrusion in the grounding zone as a target for repeat-pass surveys. We also discuss the distinct implications of our suggested approaches for instrument, platform and survey choices to combine mapping and repeat-pass surveys across the time scales of ice-sheet change. This article is part of the Theo Murphy meeting issue 'Next generation ice-sheet bed measurements'.","url":"https://doi.org/10.1098/rsta.2024.0548","contact":"Dustin M. Schroeder, Ellianna Abrahams, Anna L. Broome, Winnie Chu, Riley Culberg, Eliza J. Dawson, Emma MacKie, Daniel F. May","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":340,"type":"publication","title":"Non-Negative Matrix Factorization for Event Data","institution":"arXiv","country":"International","city":"","latitude":null,"longitude":null,"tags":"arxiv,publication,preprint","description":"Continuous-time event data, in which entities emit instantaneous events over time, arises naturally across many domains such as neuroscience, seismology, and social networks. Non-negative matrix factorization (NMF) is a natural tool to uncover interpretable structure in such data, but it has so far only been applied after binning or smoothing the entity-level counting measures. This preprocessing step comes with the risk of erasing entity-level heterogeneities and fine-grained temporal features. In this paper, we introduce EventNMF, a continuous-time non-negative factorization model that operates directly on event times: each entity's events are modeled as a Poisson process whose intensity factorizes through a non-negative B-spline basis, and a simple estimation procedure recovers interpretable temporal templates shared across entities. The resulting method is mathematically principled, easy to implement, and computationally efficient. We further show that standard binned-count approaches arise as the special case of degree-zero splines, explore bias-variance tradeoffs and compare against existing methods on a synthetic latent factor model, and demonstrate the effectiveness of Even","url":"http://arxiv.org/abs/2606.06205v1","contact":"","deadline":"2026-06-04T14:12:00Z","source":"arXiv","priority":5,"created_at":"2026-06-27T21:27:28.763349","quality_score":73,"quality_reason":"priority=5, has_url, trusted_source, good_description, detailed_description, good_tags"},{"id":1255,"type":"publication","title":"Nonparametric Inference on Treatment-biomarker Interaction Based on Probability Index","institution":"Statistica Sinica","country":"International","city":"","latitude":null,"longitude":null,"tags":"crossref,publication,doi,scientific literature","description":"Crossref publication metadata. Journal: Statistica Sinica. Authors: Zehui Wang, Yanglei Song, Wenyu Jiang, Dongsheng Tu. Year: 2028.","url":"https://doi.org/10.5705/ss.202025.0076","contact":"Zehui Wang, Yanglei Song, Wenyu Jiang, Dongsheng Tu","deadline":"2028","source":"Crossref","priority":6,"created_at":"2026-06-27T21:51:40.076393","quality_score":0,"quality_reason":""},{"id":350,"type":"publication","title":"Not All Actions Are Equal: Rethinking Conditioning for Dexterous World Model","institution":"arXiv","country":"International","city":"","latitude":null,"longitude":null,"tags":"arxiv,publication,preprint","description":"Recent advances in action-conditioned world models show promising progress in modeling complex interactions and forecasting future states under diverse action sequences. While these models are often driven by stronger visual representations and model capacity, action conditioning itself remains underexplored. Most existing approaches compress the entire action sequence into a single representation, which works well for low-DoF control but becomes less reliable in high-DoF scenarios. We observe that high-DoF dexterous actions are inherently heterogeneous, spanning multiple orders of magnitude, where large-scale motions coexist with subtle but important signals. When uniformly aggregated, optimization exhibits an imbalance across action components, which hinders the modeling of fine-grained effects and affects action fidelity. We therefore propose DexAC-WM, which treats action conditioning as a structured process rather than global compression. DexAC preserves dimension-level semantics via action tokenization and aligns action signals with visual dynamics through local refinement and global modulation. To address the limited high-level semantic grounding in existing world models, we ","url":"http://arxiv.org/abs/2606.27325v1","contact":"","deadline":"2026-06-25T17:36:35Z","source":"arXiv","priority":5,"created_at":"2026-06-27T21:27:28.763349","quality_score":73,"quality_reason":"priority=5, has_url, trusted_source, good_description, detailed_description, good_tags"},{"id":443,"type":"publication","title":"Observed positive feedback between surface ablation and crevasse formation drives glacier acceleration and potential surge","institution":"University of Oslo, Norwegian Polar Institute, Norsar, Centre National de la Recherche Scientifique, Institut des Géosciences de l'Environnement, Université Gustave Eiffel","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,glacier,surge,geology,crevasse,meltwater,acceleration","description":"Sudden glacier acceleration and instability, e.g. surges, strongly influence glacier ice loss. However, lack of in-situ observations of the involved processes hampers our ability to understand, quantify and model such a role. We present an analysis of the initiation of a surge (Kongsvegen glacier, Svalbard), focusing on the interplay between climatic and glacier-specific drivers. We integrate two decades of in-situ observations (GNSS, borehole and surface seismometers) with runoff simulations, and remotely sensed surface-elevation changes. We show that initial glacier thinning led to localized acceleration and crevassing. Then, we show that stronger surface melt enabled meltwater to reach the glacier bed. This input promotes high basal water pressure and glacier sliding, and in turn further surface crevassing. Our observations suggest that this positive feedback leads to the expansion of the initially localized instability. Our findings highlight mechanisms that could trigger glacier instabilities under a warming atmosphere beyond the High Arctic.","url":"https://doi.org/10.1038/s41467-025-66349-9","contact":"Ugo Nanni, Coline Bouchayer, Henning Åkesson, Pierre-Marie Lefeuvre, Erik Schytt Mannerfelt, Andreas Köhler, Olivier Gagliardini, Jack Kohler","deadline":"2025","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":788,"type":"publication","title":"Ocean stratification and tides control basal melting at the Ross Ice Shelf Grounding Zone","institution":"Statistics New Zealand, University of Auckland, Education New Zealand, Victoria University of Wellington, Georgia Institute of Technology, Cornell University, Swiss Federal Institute for Forest, Snow and Landscape Research, ETH Zurich, Honeybee Robotics (United States)","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,geology,stratification (seeds),oceanography,meltwater,ice shelf,sea ice","description":"The interactions among ice, ocean, and seafloor in Antarctic grounding zones hold major implications for global sea level rise over the coming century and beyond. Meltwater buoyancy means that grounding zone conditions influence basal boundary layer throughout the entire cavity. Because of the difficulty of direct access, grounding zone ocean environments have been sampled only a handful of times and then usually only as a brief data snapshot. Here, we present ocean data from the Kamb Ice Stream grounding zone of the Ross Ice Shelf that reveal a consistently stratified 30-meter-thick water column beneath nearly 600 meters of ice and snow. Warmer inflowing seawater is vertically separated from an overlying colder outflowing mixture of seawater and glacial meltwater. The 10-month long timeseries of stratification reveals that this layering is resilient but variable, with internal wave activity resulting in frequent mixing between the two layers that suggests a mechanistic underpinning for the grounding zone as a distinct region within the cavity.","url":"https://doi.org/10.1126/sciadv.ady8474","contact":"Craig Stevens, Craig Stewart, Natalie Robinson, Peter Washam, Huw J. Horgan, Justin Lawrence, Peter de Joux, B. E. Schmidt","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":371,"type":"publication","title":"Offset-continuation-trajectory stacking based on common-reflection-point kinematics for five-dimensional prestack dataset regularization and enhancement","institution":"arXiv","country":"International","city":"","latitude":null,"longitude":null,"tags":"arxiv,publication,preprint","description":"Prestack seismic data regularization and enhancement are critical steps for reliable imaging and inversion, particularly in five-dimensional (5D) dataset geometries affected by irregular sampling, noise contamination, and incomplete spatial coverage. These limitations often degrade event continuity and compromise the physical consistency of conventional interpolation methods. This study introduces a physics-informed framework for 5D prestack dataset reconstruction based on a multi-parameter common-reflection-point (CRP) traveltime stacking operator. The proposed offset-continuation-trajectory (OCT) operator derives coherent stacking trajectories from wavefront propagation, isochronous surface geometry, specular reflection, and diffraction kinematics. All kinematic parameters are estimated directly from the data through a global coevolutionary optimization strategy. The method reconstructs missing traces and enhances spatial continuity by stacking seismic events along physically consistent traveltime surfaces, preserving both reflection and diffraction kinematics. Applications to synthetic and field datasets demonstrate improved signal-to-noise ratio, enhanced structural continuity,","url":"http://arxiv.org/abs/2606.24760v1","contact":"","deadline":"2026-06-23T16:18:33Z","source":"arXiv","priority":5,"created_at":"2026-06-27T21:27:28.763349","quality_score":73,"quality_reason":"priority=5, has_url, trusted_source, good_description, detailed_description, good_tags"},{"id":374,"type":"publication","title":"On the classification of triggers of dynamic processes in geophysics","institution":"arXiv","country":"International","city":"","latitude":null,"longitude":null,"tags":"arxiv,publication,preprint","description":"In geophysics, the problem of classifying triggers of dynamic processes in the lithosphere, hydrosphere, atmosphere, ionosphere and magnetosphere has arisen and needs to be solved. Triggers that induce catastrophic events, such as destructive earthquakes, require special attention. Classification is necessary in order to express the diversity of triggers in a limited number of ordered and well-identifiable species. This paper proposes a project for collective work on the systematization of triggers, i.e., the formation of a unified classification and nomenclature. A simplified (basic) and extended classification table are proposed. The basic matrix uses the principle of binary opposition. The matrix contains three categories of descending rank: type (natural, artificial), class (endogenous, exogenous) and specie (periodic, aperiodic). Three additional categories have been added to the expanded classification table. This results in 128 trigger varieties. The heuristic significance of the classification of triggers is emphasized. New phenomena discovered during the classification process are indicated: excitation of a strong aftershock by a round-the-world seismic echo, modulation of","url":"http://arxiv.org/abs/2606.21964v1","contact":"","deadline":"2026-06-20T09:40:06Z","source":"arXiv","priority":5,"created_at":"2026-06-27T21:27:28.763349","quality_score":73,"quality_reason":"priority=5, has_url, trusted_source, good_description, detailed_description, good_tags"},{"id":333,"type":"publication","title":"Once more: Leaky MHD waves in coronal magnetic flux tubes","institution":"arXiv","country":"International","city":"","latitude":null,"longitude":null,"tags":"arxiv,publication,preprint","description":"By a detailed comparison of leaky magnetohydrodynamic waves in coronal magnetic flux tubes with leaky electromagnetic waves in dielectric media it is shown that the latter kind may be called quasi-normal modes, since they can be regularised by a normalisation which systematically cuts off the contribution of the external homogeneous region, whereas such a possibility is forbidden for the former kind by the conservation of magnetic flux. Consequently, leaky magnetohydrodynamic waves cannot be systematically applied to coronal seismology, i.e. to the inverse spectral problem of determining the different equilibrium distributions of the fields by comparing the spectra they produce with the observed ones.","url":"http://arxiv.org/abs/2606.20019v1","contact":"","deadline":"2026-06-18T09:49:39Z","source":"arXiv","priority":5,"created_at":"2026-06-27T21:27:28.763349","quality_score":73,"quality_reason":"priority=5, has_url, trusted_source, good_description, detailed_description, good_tags"},{"id":325,"type":"publication","title":"Opportunities for Gravitational Wave Physics at the South Pole","institution":"OpenAlex","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,gravitational wave,physics,atom interferometer,interferometry,astronomical interferometer,gravitational-wave observatory","description":"Atom interferometers represent a promising approach for gravitational wave detection in the decihertz frequency band, complementary to existing light-based detectors. The South Pole offers unique advantages for such experiments: exceptionally low seismic noise, established infrastructure for large scientific projects, and a location that strengthens gravitational wave source localization through global triangulation. Here we discuss the scientific case and practical considerations for deploying a long-baseline atom interferometer at the South Pole, which has the potential to expand the global network of gravitational wave detectors while enabling precision tests of fundamental physics.","url":"https://openalex.org/W7161452990","contact":"CA Argüelles, M. DuVernois, P. W. Graham, T. Kovachy, J. Mitchell","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:18:32.932503","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1466,"type":"publication","title":"Optical Gemmological Microscopy Analysis of Three Kangxi-Period Seal Paste Boxes (印色盒 Yínse hé) from a Private Scholarly Collection","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,publication","description":"Publication. Abstract
\n
example: expored links in old version
import { Thermometer, Droplets, Clock, Beaker, FlaskConical, Zap } from 'lucide-react';
// State for coffee body
const [coffeeTemp, setCoffeeTemp] = useState(85.0);
const [coffeeVolume, setCoffeeVolume] = useState(250.0);
const [coffeePh, setCoffeePh] = useState(5.0);
const [additiveTemp, setAdditiveTemp] = useState(5.0);
const [additiveVolume, setAdditiveVolume] = useState(50.0);
const [additiveFat, setAdditiveFat] = useState(15.0);
const [timeElapsed, setTimeElapsed] = useState(30.0);
const [mixingIntensity, setMixingIntensity] = useState(5.0);
const [ambientTemp,","url":"https://doi.org/10.5281/zenodo.20968834","contact":"Stone, Travis Raymond-Charlie","deadline":"2026-06-27","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":1144,"type":"publication","title":"Recent Trends and Regime Shifts in Arctic Coastal Temperatures: Evidence of AMOC Slowing?","institution":"Kola Science Centre","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,arctic,climatology,environmental science,archipelago,global warming,climate change","description":"This study analyzes surface air temperature (SAT) trends at 158 stations located on or above the Arctic Circle over the 2000–2024 period, aiming to assess whether recent temperature shifts could serve as indirect indicators of a slowing Atlantic Meridional Overturning Circulation (AMOC). Regression analysis reveals that only 40% of stations show statistically significant warming trends (p < 0.05), while 33% exhibit no significant trend. Applying the Pettitt and Buishand tests, we detect abrupt regime shifts at 38 stations, with breakpoints concentrated between 2009 and 2014. Notably, 36 of these stations display a weakening of the warming trend after the breakpoint: at 13 stations (including key Arctic archipelagos and the White Sea coast), an initial increase shifts to a decrease; at 17 stations, warming continues but at a slower rate; and at 6 stations (near the Bering Strait), a decrease intensifies. These spatial patterns suggest a potential fingerprint of AMOC slowdown, consistent with recent modeling studies that predict cooling in northwestern Europe and possible Little Ice Age-type environmental conditions. Our findings have implications for assessing future Arctic navigation, coastal infrastructure, and resource extraction under changing climate regimes.","url":"https://doi.org/10.3390/geosciences16060239","contact":"Е. А. Касаткина, О. И. Шумилов, Dmitry V. Makarov","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":373,"type":"publication","title":"Reconstructing GRACE Terrestrial Water Storage with Spatio-Temporal Graph Neural Networks: An Application to South America","institution":"arXiv","country":"International","city":"","latitude":null,"longitude":null,"tags":"arxiv,publication,preprint","description":"Terrestrial water storage (TWS) integrates snow, soil moisture, surface water, and groundwater and is a key indicator of how climate variability and human activity reshape the global water cycle. The GRACE and GRACE-FO satellite missions provide the only direct, globally consistent observations of TWS change, but their record only begins in 2002 which is too short for many climate-scale analyses. We present a deep learning application that reconstructs monthly GRACE-like TWS anomalies (TWSA) back to 1940 by learning the relationship between daily ERA5 meteorological forcing (precipitation, evapotranspiration, runoff) and monthly GRACE observations. In contrast to prior reconstruction approaches based on grid-cell-wise regression, CNNs, or LSTMs, we adapt a multi-variate time series graph neural network (MTGNN) architecture, which was originally developed for mobility and traffic forecasting on urban sensor networks to this satellite-geodesy task. Spatial dependencies are encoded in a static, interpretable hybrid adjacency matrix that combines geodesic proximity with lagged correlations of climatic time series, capturing both local hydrological coupling and large-scale teleconnectio","url":"http://arxiv.org/abs/2606.23833v1","contact":"","deadline":"2026-06-22T18:15:58Z","source":"arXiv","priority":5,"created_at":"2026-06-27T21:27:28.763349","quality_score":73,"quality_reason":"priority=5, has_url, trusted_source, good_description, detailed_description, good_tags"},{"id":681,"type":"publication","title":"Recovery of Strength in Thermally Cracked Freshwater and Salt-Water Ice","institution":"Dartmouth College","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,flexural strength,cracking,sea ice,compressive strength,geology,materials science","description":"Abstract. The integrity of ocean and lake ice covers is increasingly threatened by climate change, which reduces ice extent and promotes breakup. In addition to thinner ice and larger waves, thermal cracking may also contribute to ice cover failure. This study investigates the impact of thermal cracking on the flexural strength of freshwater and sea ice. Laboratory experiments show that when a narrow region of ice is thermally shocked, the flexural strength of both freshwater and sea ice initially decreases but subsequently recovers completely. In contrast, when the entire surface is thermally shocked, strength recovery is only partial in freshwater ice, while sea ice again fully recovers its strength. Repeated cycles of cracking followed by healing do not affect the recovered flexural strength. Additional experiments involving creep demonstrate that compressive stress enhances healing, highlighting the role of ice sintering in strength recovery. The differing behavior between localized and full-surface cracking is attributed to residual compressive stresses that develop during healing when only a narrow region is shocked. Rapid healing observed in sea ice is likely facilitated by its porous structure and the presence of brine, suggesting that natural sea ice may retain significant mechanical integrity even after thermal cracking.","url":"https://doi.org/10.5194/egusphere-2026-2464","contact":"Andrii Murdza, E. M. Schulson, Carl E. Renshaw","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1207,"type":"publication","title":"Redefining ‘antarctic ambassadorship’: a systematic review and conceptual clarification","institution":"University of Groningen, Wageningen University & Research","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,publication,obligation,environmental ethics,meaning (existential),sociology,politics,sustainability","description":"The concept of “Antarctic ambassadorship” suggests that visiting Antarctica inspires tourists to advocate for environmental protection. However, its definition and measurement remain unclear, limiting the ability to assess the true impact of polar travel. To address this gap, we conduct a systematic literature review on Antarctic ambassadorship through the lens of Value-Belief-Norm (VBN) theory. This research provides two critical contributions to the field. First, it clarifies the meaning of “ambassadorship” by mapping the psychological transformation from biospheric values to a felt moral obligation to act, and subsequently to pro-environmental actions. Specifically, it shows how witnessing environmental threats (problem awareness), connecting one’s personal footprint to those threats (ascribed responsibility), and believing that one can act to reduce them (outcome efficacy) are catalyzed by a deep emotional connection to the landscape, triggering a moral commitment to protect the region. Second, it proposes a novel framework that operationalizes ambassadorship behaviour by categorizing it into three distinct domains: sustainable living practices, everyday environmental activism, and political and societal engagement. By separating internal drivers from observable actions, our VBN-based framework resolves conceptual confusion and supports both empirical research on ambassadorship and the development of interventions that encourage verifiable environmental protection behavio","url":"https://doi.org/10.1080/09669582.2026.2686843","contact":"Silpa Saila Kumar, Anne M. van Valkengoed, Linda Steg","deadline":"2026","source":"OpenAlex","priority":6,"created_at":"2026-06-27T21:27:30.873646","quality_score":83,"quality_reason":"priority=6, has_url, trusted_source, good_description, detailed_description, good_tags, has_contact_or_authors"},{"id":1474,"type":"publication","title":"Remispora maritima Linder","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,taxonomic treatment,Biodiversity,Taxonomy,Fungi,Ascomycota,Sordariomycetes,Microascales,Halosphaeriaceae,Remispora,Remispora maritima","description":"Taxonomic treatment.
Prepared by Jeffrey D Walker, PhD (Walker Environmental Research LLC) for USEPA Office of Research and Development (ORD)\n
\npalimpsestr 0.24.0
\n⚠️ Behaviour change
\n\n
\nbic + 2 * sum(entropy) (previously bic - 2 * sum(entropy)). With the lower-is-better BIC convention the entropy term must be added so that overlapping/fuzzy partitions are penalised (Biernacki, Celeux & Govaert 2000); the previous sign rewarded them. compare_k() ICL values change accordingly. BIC, PDI, and every case-study figure are unaffected (ICL is not used in any manuscript figure), so existing K-selection conclusions stand.Bug fixes
\n\n
\nicl == bic + 2 * sum(entropy) and icl >= bic.Other changes
\n\n
archaeo_sim() now returns the simulated date bounds date_min and da","url":"https://doi.org/10.5281/zenodo.20849361","contact":"enzo","deadline":"2026-06-25","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":1445,"type":"publication","title":"fiesta-galaxy-meltponds-eo","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,software,galaxy,image-analysis,cross-discipline,earth-observation,cryosphere,supraglacial-lakes,melt-ponds,sentinel-2,NDWI,FIESTA","description":"Software. A cross-discipline OSCARS-FIESTA example: the standard Galaxy bioimage-analysis workflow (threshold, label, count, measure) run unchanged on Sentinel-2 imagery to map and count supraglacial melt ponds on the Greenland ice sheet. Uses only deployed imgteam tools plus an NDWI-ice band-math step - no new tool development.","url":"https://doi.org/10.5281/zenodo.20943837","contact":"Fouilloux, Anne","deadline":"2026-06-27","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":1453,"type":"publication","title":"pyhydra: a modular Python library for hydrological and climate analysis","institution":"Zenodo","country":"International","city":"","latitude":null,"longitude":null,"tags":"zenodo,open science,software,hydrology,flood modelling,climate analysis,stochastic rainfall,extreme value analysis,HEC-RAS,SFINCS,HEC-HMS,Manning roughness,Python","description":"Software. pyhydra is a modular Python library for hydrological and climate analysis. It covers the full pipeline from raw data acquisition to stochastic analysis, flood modelling and uncertainty quantification, integrating data sources, extreme value analysis, stochastic generation, HEC-HMS, HEC-RAS and SFINCS automation, and Manning roughness Monte Carlo sensitivity.","url":"https://doi.org/10.5281/zenodo.20932555","contact":"Navas Fernández, Salvador","deadline":"2026-06-26","source":"Zenodo","priority":6,"created_at":"2026-06-27T21:51:47.277781","quality_score":0,"quality_reason":""},{"id":20,"type":"researcher","title":"Luke Copland","institution":"University of Ottawa","country":"Canada","city":"Ottawa","latitude":45.4215,"longitude":-75.6972,"tags":"arctic,glaciers,remote sensing","description":"Good target for Arctic glaciers and remote sensing.","url":"https://www.uottawa.ca/","contact":"","deadline":"","source":"public profile","priority":7,"created_at":"2026-06-27T21:06:45.236437","quality_score":78,"quality_reason":"priority=7, has_url, official_like_url, good_tags, high_value_type"},{"id":13,"type":"researcher","title":"Florent Gimbert","institution":"IGE Grenoble","country":"France","city":"Grenoble","latitude":45.1885,"longitude":5.7245,"tags":"cryoseismology,glacier hydrology,seismic noise","description":"Strong contact for cryoseismology, glacier dynamics and subglacial hydrology.","url":"https://www.ige-grenoble.fr/","contact":"","deadline":"","source":"public profile","priority":10,"created_at":"2026-06-27T21:06:45.236437","quality_score":83,"quality_reason":"priority=10, has_url, official_like_url, good_tags, high_value_type"},{"id":16,"type":"researcher","title":"Olaf Eisen","institution":"AWI","country":"Germany","city":"Bremerhaven","latitude":53.5396,"longitude":8.5809,"tags":"glaciology,radar,antarctica,greenland","description":"Polar glaciology researcher working on ice sheets and geophysical observations.","url":"https://www.awi.de/en/science/geosciences/glaciology.html","contact":"","deadline":"","source":"public profile","priority":9,"created_at":"2026-06-27T21:06:45.236437","quality_score":83,"quality_reason":"priority=9, has_url, official_like_url, good_tags, high_value_type"},{"id":401,"type":"researcher","title":"& contributors","institution":"Royal Observatory of Belgium","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,author,publication-linked,polar science","description":"Author appearing in OpenAlex results for: cryoseismology. Related publication: Belgian Array and Mobile Seismic Network","url":"","contact":"","deadline":"","source":"OpenAlex","priority":4,"created_at":"2026-06-27T21:27:30.873646","quality_score":43,"quality_reason":"priority=4, trusted_source, good_tags, high_value_type"},{"id":391,"type":"researcher","title":"A E Volvach","institution":"Crimean Astrophysical Observatory, Institute of the Earth’s Crust","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,author,publication-linked,polar science","description":"Author appearing in OpenAlex results for: cryoseismology. Related publication: Deterministic structures in functionals of Baikal ice deformations","url":"","contact":"","deadline":"","source":"OpenAlex","priority":4,"created_at":"2026-06-27T21:27:30.873646","quality_score":53,"quality_reason":"priority=4, trusted_source, good_description, good_tags, high_value_type"},{"id":861,"type":"researcher","title":"A Riaz","institution":"OpenAlex","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,author,publication-linked,polar science","description":"Author appearing in OpenAlex results for: glacier archaeology. Related publication: First implementation of Tunnel Seismic Prediction in the Pakistani Himalayas: A case study from the Diamer Basha Dam Project (DBDP)","url":"","contact":"","deadline":"","source":"OpenAlex","priority":4,"created_at":"2026-06-27T21:27:30.873646","quality_score":53,"quality_reason":"priority=4, trusted_source, good_description, good_tags, high_value_type"},{"id":924,"type":"researcher","title":"A V Tetenkin","institution":"Irkutsk National Research Technical University, Institute of the Earth’s Crust","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,author,publication-linked,polar science","description":"Author appearing in OpenAlex results for: glacier archaeology. Related publication: Paleogeographic reconstruction of the formation of the first terrace of the Vitim River in the context of the evolution of the Mamakan Geoarchaeological Region","url":"","contact":"","deadline":"","source":"OpenAlex","priority":4,"created_at":"2026-06-27T21:27:30.873646","quality_score":53,"quality_reason":"priority=4, trusted_source, good_description, good_tags, high_value_type"},{"id":843,"type":"researcher","title":"A. Andrews","institution":"University of Southampton, PragmatIC (United Kingdom), University of Bologna","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,author,publication-linked,polar science","description":"Author appearing in OpenAlex results for: subglacial hydrology seismic. Related publication: The Development of a Low Power GNSS System, as Part of a Drone Assisted Environmental Sensor Network for a Glacial Environment","url":"","contact":"","deadline":"","source":"OpenAlex","priority":4,"created_at":"2026-06-27T21:27:30.873646","quality_score":53,"quality_reason":"priority=4, trusted_source, good_description, good_tags, high_value_type"},{"id":1036,"type":"researcher","title":"A. Carter","institution":"University of Wisconsin–Madison, Scripps Institution of Oceanography, Princeton University, University of California San Diego, Oregon State University, Woods Hole Oceanographic Institution, University of Washington, Earth and Space Research, Dartmouth College","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,author,publication-linked,polar science","description":"Author appearing in OpenAlex results for: Greenland ice sheet geophysics. Related publication: Dust Record from Allan Hills Blue Ice: Towards Extending the Archive to 4000 ka","url":"","contact":"","deadline":"","source":"OpenAlex","priority":4,"created_at":"2026-06-27T21:27:30.873646","quality_score":53,"quality_reason":"priority=4, trusted_source, good_description, good_tags, high_value_type"},{"id":403,"type":"researcher","title":"A. E. Volvach","institution":"Crimean Astrophysical Observatory, Institute of the Earth’s Crust","country":"International","city":"","latitude":null,"longitude":null,"tags":"openalex,author,publication-linked,polar science","description":"Author appearing in OpenAlex results for: cryoseismology. 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