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...
Published in: | Geology |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
GSA, Geological Society of America
2011
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Subjects: | |
Online Access: | https://oceanrep.geomar.de/id/eprint/21249/ https://doi.org/10.1130/G31677.1 |