Changing hydrographic structures across the Lazarev Sea
Deep water originating in the North Atlantic is transported across theAntarctic Circumpolar Current by eddies and enters the Weddell Gyresouth of Africa. As it does so it rises up from mid depth towards thesurface. The separate temperature and salinity maxima, the Upperand Lower Deep Waters, converg...
Main Authors: | , , |
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Format: | Conference Object |
Language: | unknown |
Published: |
2006
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Subjects: | |
Online Access: | https://epic.awi.de/id/eprint/16548/ https://hdl.handle.net/10013/epic.26431 |