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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.; 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.

Full text not available from this repository.
Item Type: Publication - Article
Additional Keywords: NADW, CIRCUMPOLAR DEEP WATER, SEDIMENTS, NEODYMIUM ISOTOPES
Date made live: 10 Jun 2004 +0 (UTC)
URI: http://nora.nerc.ac.uk/id/eprint/106046

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