Punctuated shutdown of Atlantic Meridional Overturning Circulation during Greenland Stadial 1
The Greenland Stadial 1 (GS-1; ~12.9 to 11.65 kyr cal BP) was a period of North Atlantic cooling, thought to have been initiated by North America fresh water runoff that caused a sustained reduction of North Atlantic Meridional Overturning Circulation (AMOC), resulting in an antiphase temperature re...
| Główni autorzy: | , , , , , , , , , , , , , , , |
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| Format: | Journal article |
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Nature Publishing Group: Open Access Journals - Option C
2016
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