Oceanic Wind-driven Circulation
Oceanic Wind-Driven Circulation is a theoretical framework in physical oceanography that describes the large-scale movement of surface ocean waters resulting from the direct action of wind stress on the sea surface, differentiated by its reliance on Ekman dynamics to explain the vertical and horizontal redistribution of momentum and mass in the upper ocean.
549
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37.5K
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1.2K
Authors
427
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2017–2026
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549
ON THE WIND-DRIVEN OCEAN CIRCULATION
Walter Munk · Journal of Meteorology · 1950 · 944 citations · Full text
James R. Luyten, Joseph Pedlosky, Henry Stommel · Journal of Physical Oceanography · 1983 · 851 citations
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Woods Hole Oceanographic Institution, United States
9 publications · 455 citations
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Woods Hole Oceanographic Institution
Falmouth, United States
20 h-index
58 publications
5.4K citations

Scripps Institution of Oceanography
La Jolla, United States
18 h-index
29 publications
2.9K citations
Massachusetts Institute of Technology
Cambridge, United States
17 h-index
26 publications
3.4K citations

University of Hawaiʻi at Mānoa
Honolulu, United States
16 h-index
34 publications
3.8K citations

Centre National de la Recherche Scientifique
Paris, France
15 h-index
38 publications
2.1K citations
University of Miami
Coral Gables, United States
13 h-index
33 publications
2K citations
Oregon State University
Corvallis, United States
13 h-index
39 publications
1.9K citations

Ocean University of China
Qingdao, China
11 h-index
22 publications
983 citations
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120 publications · 7.1K citations
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JGR · 65 publications · 6.2K citations
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18 publications · 1.9K citations
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21 publications · 1.3K citations
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19 publications · 873 citations
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