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


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.

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Item Type: Article
Keywords: NADW, CIRCUMPOLAR DEEP WATER, SEDIMENTS, NEODYMIUM ISOTOPES
Subjects: Q Science > QE Geology
G Geography. Anthropology. Recreation > GC Oceanography
Divisions: University Structure - Pre August 2011 > National Oceanography Centre (NERC)
University Structure - Pre August 2011 > School of Ocean & Earth Science (SOC/SOES)
ePrint ID: 6046
Date :
Date Event
2001Published
Date Deposited: 10 Jun 2004
Last Modified: 31 Mar 2016 11:10
URI: http://eprints.soton.ac.uk/id/eprint/6046

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