Wind-driven Overturning
Wind-Driven Overturning is a meridional overturning circulation mechanism distinguished by its primary dependence on surface wind stress to induce large-scale oceanic upwelling and downwelling, thereby shaping the meridional transport of water masses in the upper ocean.
108
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8.1K
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303
Authors
161
Institutions
Publications per year
2017–2026
23
Variants
Wind-driven Meridional Overturning Circulation
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Robert Hallberg, Anand Gnanadesikan · Journal of Physical Oceanography · 2006 · 474 citations · Full text
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NOAA Atlantic Oceanographic and Meteorological Laboratories, United States
6 publications · 768 citations
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National Oceanography Centre
Southampton, United Kingdom
10 h-index
50 publications
5.1K citations

Scripps Institution of Oceanography
La Jolla, United States
9 h-index
13 publications
949 citations
Massachusetts Institute of Technology
Cambridge, United States
8 h-index
15 publications
1.7K citations
NOAA Atlantic Oceanographic and Meteorological Laboratories
Miami, United States
8 h-index
27 publications
3.7K citations
University of Miami
Coral Gables, United States
7 h-index
22 publications
3.1K citations
Max Planck Institute for Meteorology
Hamburg, Germany
7 h-index
27 publications
3.3K citations

UNSW Sydney
Sydney, Australia
6 h-index
12 publications
1.1K citations

Potsdam Institute for Climate Impact Research
Potsdam, Germany
6 h-index
10 publications
718 citations
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31 publications · 2.9K citations
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11 publications · 497 citations
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8 publications · 475 citations
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7 publications · 711 citations
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7 publications · 390 citations
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