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 fl ow 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: | English |
Published: |
2011
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Subjects: | |
Online Access: | https://hdl.handle.net/1983/d0432426-9019-4556-8d3f-5c2ac8ba804c https://research-information.bris.ac.uk/en/publications/d0432426-9019-4556-8d3f-5c2ac8ba804c https://doi.org/10.1130/G31677.1 http://geology.gsapubs.org/content/39/6/515 |