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Radar for Europa assessment and sounding: ocean to near-surface (REASON)
DD Blankenship, A Moussessian, E Chapin… - Space science …, 2024 - Springer
Abstract The Radar for Europa Assessment and Sounding: Ocean to Near-surface
(REASON) is a dual-frequency ice-penetrating radar (9 and 60 MHz) onboard the Europa …
(REASON) is a dual-frequency ice-penetrating radar (9 and 60 MHz) onboard the Europa …
Antarctic sedimentary basins and their influence on ice‐sheet dynamics
Abstract Knowledge of Antarctica's sedimentary basins builds our understanding of the
coupled evolution of tectonics, ice, ocean, and climate. Sedimentary basins have properties …
coupled evolution of tectonics, ice, ocean, and climate. Sedimentary basins have properties …
Radar internal reflection horizons from multisystem data reflect ice dynamic and surface accumulation history along the Princess Ragnhild Coast, Dronning Maud …
Ice shelves, which regulate ice flow from the Antarctic ice sheet towards the ocean, are
shaped by spatiotemporal patterns of surface accumulation, surface/basal melt and ice …
shaped by spatiotemporal patterns of surface accumulation, surface/basal melt and ice …
Sediment freeze‐on and transport near the onset of a fast‐flowing glacier in East Antarctica
S Franke, M Wolovick, R Drews… - Geophysical …, 2024 - Wiley Online Library
Understanding the material properties and physical conditions of basal ice is crucial for a
comprehensive understanding of Antarctic ice‐sheet dynamics. Yet, direct data are sparse …
comprehensive understanding of Antarctic ice‐sheet dynamics. Yet, direct data are sparse …
Coastal bathymetry in central Dronning Maud Land controls ice shelf stability
H Eisermann, G Eagles, W Jokat - Scientific Reports, 2024 - nature.com
Abstract Knowledge of the bathymetry of Antarctica's margins is crucial for models and
interpretations of ice-ocean interactions and their influence on ongoing and future sea level …
interpretations of ice-ocean interactions and their influence on ongoing and future sea level …
[HTML][HTML] Alpine topography of the Gamburtsev Subglacial Mountains, Antarctica, mapped from ice sheet surface morphology
Landscapes buried beneath the Antarctic Ice Sheet preserve information about the geologic
and geomorphic evolution of the continent both before and during the wide-scale glaciation …
and geomorphic evolution of the continent both before and during the wide-scale glaciation …
Stochastic simulations of bed topography constrain geothermal heat flow and subglacial drainage near Dome Fuji, East Antarctica
Topographic variability beneath ice sheets regulates ice flow, basal melting, refreezing
processes, and meltwater drainage. The preservation of old ice layers and basal ice …
processes, and meltwater drainage. The preservation of old ice layers and basal ice …
Ice thickness and bed topography of Jostedalsbreen ice cap, Norway
MK Gillespie, LM Andreassen, M Huss… - Earth System …, 2024 - essd.copernicus.org
We present an extensive dataset of ice thickness measurements from Jostedalsbreen ice
cap, mainland Europe's largest glacier. The dataset consists of more than 351 000 point …
cap, mainland Europe's largest glacier. The dataset consists of more than 351 000 point …
Evidence of active subglacial lakes under a slowly moving coastal region of the Antarctic Ice Sheet
Active subglacial lakes beneath the Antarctic Ice Sheet provide insights into the dynamic
subglacial environment, with implications for ice-sheet dynamics and mass balance. Most …
subglacial environment, with implications for ice-sheet dynamics and mass balance. Most …
[HTML][HTML] ISMIP6-based Antarctic projections to 2100: simulations with the BISICLES ice sheet model
JF O'Neill, TL Edwards, DF Martin, C Shafer… - The …, 2025 - tc.copernicus.org
The contribution of the Antarctic Ice Sheet is one of the most uncertain components of sea
level rise to 2100. Ice sheet models are the primary tool for projecting future sea level …
level rise to 2100. Ice sheet models are the primary tool for projecting future sea level …