Dynamics of the last glacial maximum Antarctic ice-sheet and its response to ocean forcing

Retreat of the Last Glacial Maximum (LGM) Antarctic ice sheet is thought to have been initiated by changes in ocean heat and eustatic sea level propagated from the Northern Hemisphere (NH) as northern ice sheets melted under rising atmospheric temperatures. The extent to which spatial variability in...

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Bibliographic Details

Published in:	Proceedings of the National Academy of Sciences - PNAS Vol. 109; no. 40; p. 16052
Main Authors:	Golledge, Nicholas R, Fogwill, Christopher J, Mackintosh, Andrew N, Buckley, Kevin M
Format:	Journal Article
Language:	English
Published:	United States 02.10.2012
Subjects:	Antarctic Regions Computer Simulation Global Warming History, Ancient Ice Cover - chemistry Models, Theoretical Oceans and Seas Water Movements Antarctic Regions
ISSN:	1091-6490, 1091-6490
Online Access:	Get more information
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