Enrichment of silicate and CO2 and circulation of the bottom water in the Weddell Sea
Deep and bottom water from the Enderby Basin, which is strongly enriched in silicate, enters the Weddell Sea off Kapp Norvegia parallel to the coast. However, the bottom water in this region originates from the northern Weddell Sea, indicating a southward return flow of bottom water west of the prim...
Published in: | Deep Sea Research Part I: Oceanographic Research Papers |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
1998
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Subjects: | |
Online Access: | https://hdl.handle.net/11370/3a0c0f3f-2f44-4366-aa42-126deaaa945f https://research.rug.nl/en/publications/3a0c0f3f-2f44-4366-aa42-126deaaa945f https://doi.org/10.1016/S0967-0637(98)00029-6 https://pure.rug.nl/ws/files/10647288/1998DeepSeaRes1Hoppema.pdf |