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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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Main Authors: Golledge, Nicholas R., Fogwill, Christopher J., Mackintosh, Andrew N., Buckley, Kevin M.
Formáid: Artigo
Teanga:Inglês
Foilsithe: National Academy of Sciences 2012
Ábhair:
Rochtain Ar Líne:https://ncbi.nlm.nih.gov/pmc/articles/PMC3479616/
https://ncbi.nlm.nih.gov/pubmed/22988078
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1205385109
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