Weddell Sea abyssal sediments a record of Antarctic Bottom Water Flow
Deep circulation in the Weddell Sea is a clockwise gyre, with bottom water formed by mixing along the southern and western margins. Most Antarctic Bottom Water originates here, leaving the Weddell Sea to the east (depths > 4500 m) or to the north (depths < 3500 m). This paper describes two cor...
Published in: | Marine Geology |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Elsevier
1988
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Subjects: | |
Online Access: | http://nora.nerc.ac.uk/id/eprint/521736/ https://doi.org/10.1016/0025-3227(88)90032-1 |