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Increased circumpolar deep water flow in the glacial South Atlantic: the cause of apparent North Atlantic deep water weakening

Record type: Article

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Citation

Bayon, G., German, C.R., Nesbitt, R.W., Bertrand, P. and Schneider, R.R. (2001) Increased circumpolar deep water flow in the glacial South Atlantic: the cause of apparent North Atlantic deep water weakening EOS: Transactions American Geophysical Union, 82, (47, Supplement), F618-F619.

More information

Published date: 2001
Keywords: NADW, CIRCUMPOLAR DEEP WATER, SEDIMENTS, NEODYMIUM ISOTOPES

Identifiers

Local EPrints ID: 6046
URI: http://eprints.soton.ac.uk/id/eprint/6046
ISSN: 0096-3941
PURE UUID: 5604f50c-9076-45b7-8470-d35d2504734b

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Date deposited: 10 Jun 2004
Last modified: 17 Jul 2017 17:15

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Contributors

Author: G. Bayon
Author: C.R. German
Author: R.W. Nesbitt
Author: P. Bertrand
Author: R.R. Schneider

University divisions

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