Comparing a thermo-mechanical Weichselian Ice Sheet reconstruction to reconstructions based on the sea level equation: aspects of ice configurations and glacial isostatic adjustment [PDF]
In this study we compare a recent reconstruction of the Weichselian Ice Sheet as simulated by the University of Maine ice sheet model (UMISM) to two reconstructions commonly used in glacial isostatic adjustment (GIA) modelling: ICE-5G and ANU (Australian
P. Schmidt +3 more
doaj +1 more source
Hysteresis of the Antarctic Ice Sheet With a Coupled Climate‐Ice‐Sheet Model
AbstractThe stability of the Antarctic ice sheet under different fixed levels and orbital configurations is explored using a coupled climate‐ice sheet model, starting from either a pre‐industrial ice sheet or an ice‐free, isostatically rebounded geometry.
Gaëlle Leloup +4 more
openaire +5 more sources
The potential of marine ice cliff instability for Amundsen Sea glaciers revisited
Marine ice cliff instability (MICI) is the hypothesis that self-sustained retreat of ice sheets can be initiated when sufficiently tall ice cliffs are exposed.
Sainan Sun, Gudmundur Hilmar Gudmundsson
doaj +1 more source
Modelling the diversion of erratic boulders by the Valais Glacier during the last glacial maximum
In this study, a modelling approach was used to investigate the cause of the diversion of erratic boulders from Mont Blanc and southern Valais by the Valais Glacier to the Solothurn lobe during the Last Glacial Maximum (LGM). Using the Parallel Ice Sheet
GUILLAUME JOUVET +3 more
doaj +1 more source
Geothermal heat flow (GHF) influences ice sheet thermal conditions, affecting ice flow by sliding and deformation. However, GHF distribution under polar ice sheets remains poorly constrained, with few direct borehole-derived estimates and large ...
Mareen Lösing +11 more
doaj +1 more source
Simulating the Holocene evolution of Ryder Glacier, North Greenland [PDF]
The Greenland Ice Sheet's negative mass balance is driven by a sensitivity to a warming atmosphere and ocean. The fidelity of ice-sheet models in accounting for ice–ocean interaction is inherently uncertain and often constrained against recent ...
J. Barnett +15 more
doaj +1 more source
Evolution of the large-scale atmospheric circulation in response to changing ice sheets over the last glacial cycle [PDF]
We present modelling results of the atmospheric circulation at the cold periods of marine isotope stage 5b (MIS 5b), MIS 4 and the Last Glacial Maximum (LGM), as well as the interglacial.
M. Löfverström +3 more
doaj +1 more source
A technique for generating consistent ice sheet initial conditions for coupled ice sheet/climate models [PDF]
Abstract. A transient technique for generating ice sheet preindustrial initial conditions for long-term coupled ice sheet/climate model simulations is developed and demonstrated over the Greenland ice sheet using the Community Earth System Model (CESM).
J. G. Fyke, W. J. Sacks, W. H. Lipscomb
openaire +3 more sources
A facet-based numerical model to retrieve ice sheet topography from Sentinel-3 altimetry [PDF]
In this study, we present a facet-based numerical model dedicated to ice sheet radar altimetry. The model simulates Sentinel-3 UnFocused-Synthetic Aperture Radar (UF-SAR) waveforms by calculating the backscattered radar signal over the 10 m facets of the
J. Aublanc +3 more
doaj +1 more source

