Antarctic sea ice control on ocean circulation in present and glacial climates
In the modern climate, the ocean below 2 km is mainly filled by waters sinking into the abyss around Antarctica and in the North Atlantic. Paleoproxies indicate that waters of North Atlantic origin were instead absent below 2 km at the Last Glacial Maximum, resulting in an expansion of the volume oc...
| Main Authors: | , , , , , |
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| Other Authors: | |
| Format: | Article |
| Language: | English |
| Published: |
National Academy of Sciences (U.S.),
2015-01-07T20:30:32Z.
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| Subjects: | |
| Online Access: | Get fulltext |