Large-scale Wind-driven Circulation
Large-Scale Wind-Driven Circulation is a theoretical construct in physical oceanography that describes the broad, basin-scale patterns of ocean surface currents generated predominantly by the sustained forcing of global wind stress, distinguished by its geostrophic balance, curl-driven Ekman transport, and role in forming major gyres and western boundary currents.
398
Publications
28.7K
Citations
1.1K
Authors
410
Institutions
Publications per year
2017–2026
64
Parents
398
Upper-level circulation in the South Atlantic Ocean
Ray Peterson, Lothar Stramma · Progress In Oceanography · 1991 · 1.2K citations
A Simple Predictive Model for the Structure of the Oceanic Pycnocline
Anand Gnanadesikan · Science · 1999 · 557 citations
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Centre National de la Recherche Scientifique
Paris, France
14 h-index
38 publications
1.7K citations
Woods Hole Oceanographic Institution
Falmouth, United States
14 h-index
30 publications
1.9K citations
University of Washington
Seattle, United States
13 h-index
17 publications
1K citations
Massachusetts Institute of Technology
Cambridge, United States
11 h-index
15 publications
3.2K citations

Chinese Academy of Sciences
Beijing, China
11 h-index
22 publications
975 citations
University of Miami
Coral Gables, United States
11 h-index
17 publications
652 citations

Scripps Institution of Oceanography
La Jolla, United States
10 h-index
14 publications
590 citations

University of Hawaiʻi at Mānoa
Honolulu, United States
10 h-index
17 publications
2.3K citations
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53 publications · 4.2K citations
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JGR · 39 publications · 2.3K citations
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19 publications · 1.6K citations
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19 publications · 731 citations
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