Last major retreat of Antarctic ice sheets forced by sea level rise and ocean warming.
The retreat of Antarctic ice sheets during the transition from the last glacial period to the Holocene provides the most recent example of ice sheet response to major climate forcing and thus allows rates of ice sheet decay and coupling to sea level rise to be quantified. We observe through a combin...
Main Authors: | , , , , , , , , |
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Format: | Conference Object |
Language: | English |
Published: |
2009
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Subjects: | |
Online Access: | http://apo.ansto.gov.au/dspace/handle/10238/2745 |