The development of the Western Boundary Undercurrent (WBUC) in a changing climate since the beginning of the Miocene
The present deep Western Boundary Undercurrent (WBUC) at the Eirik Drift off the southern tip of Greenland is mainly fed by the overflows over the Greenland-Scotland ridge (GSR), the Denmark Strait Overflow Water (DSOW) and Iceland-Scotland Overflow Water (ISOW), respectively (Fig. 1). Interactions...
Main Authors: | , |
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Format: | Conference Object |
Language: | unknown |
Published: |
2013
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Subjects: | |
Online Access: | https://epic.awi.de/id/eprint/32221/ https://hdl.handle.net/10013/epic.40856 |