학술논문
Observed Flow Compensation Associated with the MOC at 26.5°N in the Atlantic.
Document Type
Article
Author
Source
Subject
*MERIDIONAL winds
*ATMOSPHERIC circulation
*HEAT flux
*GEOSTROPHIC wind
*GULF Stream
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*
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Language
ISSN
0036-8075
Abstract
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°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 × 106 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. [ABSTRACT FROM AUTHOR]