Document Detail

Observed flow compensation associated with the MOC at 26.5 degrees N in the Atlantic.
MedLine Citation:
PMID:  17702941     Owner:  NLM     Status:  PubMed-not-MEDLINE    
The Atlantic meridional overturning circulation (MOC), which provides one-quarter of the global meridional heat transport, is composed of a number of separate flow components. How changes in the strength of each of those components may affect that of the others has been unclear because of a lack of adequate data. We continuously observed the MOC at 26.5 degrees N for 1 year using end-point measurements of density, bottom pressure, and ocean currents; cable measurements across the Straits of Florida; and wind stress. The different transport components largely compensate for each other, thus confirming the validity of our monitoring approach. The MOC varied over the period of observation by +/-5.7 x 10(6) cubic meters per second, with density-inferred and wind-driven transports contributing equally to it. We find evidence for depth-independent compensation for the wind-driven surface flow.
Torsten Kanzow; Stuart A Cunningham; Darren Rayner; Joël J-M Hirschi; William E Johns; Molly O Baringer; Harry L Bryden; Lisa M Beal; Christopher S Meinen; Jochem Marotzke
Publication Detail:
Type:  Journal Article; Research Support, Non-U.S. Gov't; Research Support, U.S. Gov't, Non-P.H.S.    
Journal Detail:
Title:  Science (New York, N.Y.)     Volume:  317     ISSN:  1095-9203     ISO Abbreviation:  Science     Publication Date:  2007 Aug 
Date Detail:
Created Date:  2007-08-17     Completed Date:  2007-09-05     Revised Date:  -    
Medline Journal Info:
Nlm Unique ID:  0404511     Medline TA:  Science     Country:  United States    
Other Details:
Languages:  eng     Pagination:  938-41     Citation Subset:  -    
National Oceanography Centre, Empress Dock, Southampton, SO14 3ZH, UK.
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Comment In:
Science. 2007 Aug 17;317(5840):908-9   [PMID:  17702934 ]

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