A stable Faroe Bank Channel overflow 1995–2015
The Faroe Bank Channel (FBC) is the deepest passage across the Greenland–Scotland Ridge (GSR) and there is a continuous deep flow of cold and dense water passing through it from the Arctic Mediterranean into the North Atlantic and further to the rest of the world ocean. This FBC overflow is part of...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2016-11-01
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| Series: | Ocean Science |
| Online Access: | http://www.ocean-sci.net/12/1205/2016/os-12-1205-2016.pdf |