Coupled regional climate–ice-sheet simulation shows limited Greenland ice loss during the Eemian
During the last interglacial period (Eemian, 130–115 kyr BP) eustatic global sea level likely peaked at > 6 m above the present-day level, but estimates of the contribution of the Greenland Ice Sheet vary widely. Here we use an asynchronously two-way-coupled regional climate–ice-sheet model, whic...
| Main Authors: | , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2013-08-01
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| Series: | Climate of the Past |
| Online Access: | http://www.clim-past.net/9/1773/2013/cp-9-1773-2013.pdf |