A major change in North Atlantic deep water circulation 1.6 million years ago
The global ocean–climate system has been highly sensitive to the formation and advection of deep overflow water from the Nordic Seas as integral part of the Atlantic Meridional Overturning Circulation (AMOC) but its evolution over the Pliocene–Pleistocene global cooling is not fu...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2014-07-01
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| Series: | Climate of the Past |
| Online Access: | http://www.clim-past.net/10/1441/2014/cp-10-1441-2014.pdf |