Persistent Nordic deep-water overflow to the glacial North Atlantic

North Atlantic climate is very sensitive to overturning in the Greenland-Iceland-Norwegian (GIN) Seas, overflow of deep water into the North Atlantic via the Greenland-Iceland-Scotland Ridge, and compensating northward flow of warm surface water. Physical models suggest that, in the absence of such...

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Bibliographic Details
Published in:Geology
Main Authors: Crocket, K. C., Vance, D., Gutjahr, Marcus, Foster, G. L., Richards, D. A.
Format: Article in Journal/Newspaper
Language:unknown
Published: GSA, Geological Society of America 2011
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/21249/
https://doi.org/10.1130/G31677.1