A deglacial model for Antarctica: geological constraints and glaciological modelling as a basis for a new model of Antarctic glacial isostatic adjustment
We present a new reconstruction of the Antarctic Ice Sheets between 20 ka BP and the
present day. Our reconstruction is derived using a numerical model to generate a physically …
present day. Our reconstruction is derived using a numerical model to generate a physically …
Ocean tide influences on the Antarctic and Greenland ice sheets
Ocean tides are the main source of high‐frequency variability in the vertical and horizontal
motion of ice sheets near their marine margins. Floating ice shelves, which occupy about …
motion of ice sheets near their marine margins. Floating ice shelves, which occupy about …
A suite of global, cross-scale topographic variables for environmental and biodiversity modeling
Topographic variation underpins a myriad of patterns and processes in hydrology,
climatology, geography and ecology and is key to understanding the variation of life on the …
climatology, geography and ecology and is key to understanding the variation of life on the …
Modelling the climate and surface mass balance of polar ice sheets using RACMO2–Part 2: Antarctica (1979–2016)
We evaluate modelled Antarctic ice sheet (AIS) near-surface climate, surface mass balance
(SMB) and surface energy balance (SEB) from the updated polar version of the regional …
(SMB) and surface energy balance (SEB) from the updated polar version of the regional …
Estimation of the Antarctic surface mass balance using the regional climate model MAR (1979–2015) and identification of dominant processes
The Antarctic ice sheet mass balance is a major component of the sea level budget and
results from the difference of two fluxes of a similar magnitude: ice flow discharging in the …
results from the difference of two fluxes of a similar magnitude: ice flow discharging in the …
Bedmap2: improved ice bed, surface and thickness datasets for Antarctica
We present Bedmap2, a new suite of gridded products describing surface elevation, ice-
thickness and the seafloor and subglacial bed elevation of the Antarctic south of 60° S. We …
thickness and the seafloor and subglacial bed elevation of the Antarctic south of 60° S. We …
Variable temperature thresholds of melt pond formation on Antarctic ice shelves
JM van Wessem, MR van den Broeke… - Nature Climate …, 2023 - nature.com
It has been argued that the− 5° C annual mean 2 m air temperature isotherm defines a limit
of ice shelf viability on the Antarctic Peninsula as melt ponding increases at higher …
of ice shelf viability on the Antarctic Peninsula as melt ponding increases at higher …
Marine ice sheet collapse potentially under way for the Thwaites Glacier Basin, West Antarctica
Resting atop a deep marine basin, the West Antarctic Ice Sheet has long been considered
prone to instability. Using a numerical model, we investigated the sensitivity of Thwaites …
prone to instability. Using a numerical model, we investigated the sensitivity of Thwaites …
Elevation and elevation change of Greenland and Antarctica derived from CryoSat-2
V Helm, A Humbert, H Miller - The Cryosphere, 2014 - tc.copernicus.org
This study focuses on the present-day surface elevation of the Greenland and Antarctic ice
sheets. Based on 3 years of CryoSat-2 data acquisition we derived new elevation models …
sheets. Based on 3 years of CryoSat-2 data acquisition we derived new elevation models …
[HTML][HTML] What is the surface mass balance of Antarctica? An intercomparison of regional climate model estimates
We compare the performance of five different regional climate models (RCMs)(COSMO-CLM
2, HIRHAM5, MAR3. 10, MetUM, and RACMO2. 3p2), forced by ERA-Interim reanalysis, in …
2, HIRHAM5, MAR3. 10, MetUM, and RACMO2. 3p2), forced by ERA-Interim reanalysis, in …