Wind forcing of salinity anomalies in the Denmark Strait overflow
The overflow of dense water from the Nordic Seas to the North Atlantic through Denmark Strait is an important part of the global thermohaline circulation. The salinity of the overflow plume has been measured by an array of current meters across the continental slope off the coast of Angmagssalik, so...
| Main Authors: | , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2011-11-01
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| Series: | Ocean Science |
| Online Access: | http://www.ocean-sci.net/7/821/2011/os-7-821-2011.pdf |