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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: | , , , |
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| Formáid: | Artigo |
| Teanga: | Inglês |
| Foilsithe: |
National Academy of Sciences
2012
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| 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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