Exploring the impact of atmospheric forcing and basal drag on the Antarctic Ice Sheet under Last Glacial Maximum conditions
<p>Little is known about the distribution of ice in the Antarctic Ice Sheet (AIS) during the Last Glacial Maximum (LGM). Whereas marine and terrestrial geological data indicate that the grounded ice advanced to a position close to the continental-shelf break, the total ice volume is unclear. G...
Main Authors: | J. Blasco, J. Alvarez-Solas, A. Robinson, M. Montoya |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2021-01-01
|
Series: | The Cryosphere |
Online Access: | https://tc.copernicus.org/articles/15/215/2021/tc-15-215-2021.pdf |
Similar Items
-
The Antarctic Ice Sheet response to glacial millennial-scale variability
by: J. Blasco, et al.
Published: (2019-01-01) -
The sensitivity of the Greenland Ice Sheet to glacial–interglacial oceanic forcing
by: I. Tabone, et al.
Published: (2018-04-01) -
Impact of millennial-scale oceanic variability on the Greenland ice-sheet evolution throughout the last glacial period
by: I. Tabone, et al.
Published: (2019-03-01) -
Ocean-driven millennial-scale variability of the Eurasian ice sheet during the last glacial period simulated with a hybrid ice-sheet–shelf model
by: J. Alvarez-Solas, et al.
Published: (2019-06-01) -
A new approach for simulating the paleo-evolution of the Northern Hemisphere ice sheets
by: R. Banderas, et al.
Published: (2018-06-01)