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...

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Bibliographic Details
Published in:Marine Geology
Main Authors: Pudsey, Carol J., Barker, Peter F., Hamilton, Norman
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier 1988
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/521736/
https://doi.org/10.1016/0025-3227(88)90032-1