OOIR: Observatory of International Research

Papers

(The H4-Index of Cryosphere is 36. The table below lists those papers that are above that threshold based on CrossRef citation counts [max. 250 papers]. The publications cover those that have been published in the past four years, i.e., from 2020-04-01 to 2024-04-01.)

Article	Citations
ISMIP6 Antarctica: a multi-model ensemble of the Antarctic ice sheet evolution over the 21st century	191
The future sea-level contribution of the Greenland ice sheet: a multi-model ensemble study of ISMIP6	142
First evidence of microplastics in Antarctic snow	122
Historical Northern Hemisphere snow cover trends and projected changes in the CMIP6 multi-model ensemble	113
Review article: How does glacier discharge affect marine biogeochemistry and primary production in the Arctic?	107
GrSMBMIP: intercomparison of the modelled 1980–2012 surface mass balance over the Greenland Ice Sheet	104
Unprecedented atmospheric conditions (1948–2019) drive the 2019 exceptional melting season over the Greenland ice sheet	102
An enhancement to sea ice motion and age products at the National Snow and Ice Data Center (NSIDC)	95
Observed snow depth trends in the European Alps: 1971 to 2019	88
The ERA5-Land soil temperature bias in permafrost regions	84
Evaluating permafrost physics in the Coupled Model Intercomparison Project 6 (CMIP6) models and their sensitivity to climate change	76
Evaluation of long-term Northern Hemisphere snow water equivalent products	75
Review article: Earth's ice imbalance	72
Experimental protocol for sea level projections from ISMIP6 stand-alone ice sheet models	72
Diverging future surface mass balance between the Antarctic ice shelves and grounded ice sheet	66
Sudden large-volume detachments of low-angle mountain glaciers – more frequent than thought?	61
The MOSAiC ice floe: sediment-laden survivor from the Siberian shelf	57
What is the surface mass balance of Antarctica? An intercomparison of regional climate model estimates	54
Results of the third Marine Ice Sheet Model Intercomparison Project (MISMIP+)	53
Improving sub-canopy snow depth mapping with unmanned aerial vehicles: lidar versus structure-from-motion techniques	51
The catastrophic thermokarst lake drainage events of 2018 in northwestern Alaska: fast-forward into the future	51
A protocol for calculating basal melt rates in the ISMIP6 Antarctic ice sheet projections	49
Snow depth mapping from stereo satellite imagery in mountainous terrain: evaluation using airborne laser-scanning data	49
Classification of sea ice types in Sentinel-1 synthetic aperture radar images	48
The Copernicus Polar Ice and Snow Topography Altimeter (CRISTAL) high-priority candidate mission	47

MOSAiC drift expedition from October 2019 to July 2020: sea ice conditions from space and comparison with previous years	46
Sentinel-1 snow depth retrieval at sub-kilometer resolution over the European Alps	43
Consequences of permafrost degradation for Arctic infrastructure – bridging the model gap between regional and engineering scales	42
Glacier runoff variations since 1955 in the Maipo River basin, in the semiarid Andes of central Chile	41
The tipping points and early warning indicators for Pine Island Glacier, West Antarctica	40
A model for interaction between conduits and surrounding hydraulically connected distributed drainage based on geomorphological evidence from Keewatin, Canada	39
An inter-comparison of the mass budget of the Arctic sea ice in CMIP6 models	39
The Antarctic sea ice cover from ICESat-2 and CryoSat-2: freeboard, snow depth, and ice thickness	39
Calving Front Machine (CALFIN): glacial termini dataset and automated deep learning extraction method for Greenland, 1972–2019	38
Satellite passive microwave sea-ice concentration data set inter-comparison for Arctic summer conditions	38
The 2020 glacial lake outburst flood at Jinwuco, Tibet: causes, impacts, and implications for hazard and risk assessment	38
Rapid fragmentation of Thwaites Eastern Ice Shelf	36
Getz Ice Shelf melt enhanced by freshwater discharge from beneath the West Antarctic Ice Sheet	36
Thaw-driven mass wasting couples slopes with downstream systems, and effects propagate through Arctic drainage networks	36