Wind-driven Surface Transport
Wind-Driven Surface Transport is a geophysical fluid dynamics process that constitutes the net movement of surface ocean water in the uppermost layer of the ocean, distinguished by its direct response to wind stress and adherence to Ekman theory, in which the resultant transport occurs at a 90° angle relative to the direction of the prevailing wind due to the Coriolis effect.
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2017–2026
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Surface Motion of Water Induced by Wind
Irving Langmuir · Science · 1938 · 610 citations
Observed Flow Compensation Associated with the MOC at 26.5°N in the Atlantic
Torsten Kanzow, Stuart A. Cunningham, D. Rayner et al. · Science · 2007 · 226 citations
A Note on the Drag of the Sea Surface at Hurricane Winds
V. K. Makin · Boundary-Layer Meteorology · 2005 · 176 citations
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Woods Hole Oceanographic Institution
Falmouth, United States
5 h-index
8 publications
353 citations
University of Washington Applied Physics Laboratory
Seattle, United States
3 h-index
6 publications
433 citations

Scripps Institution of Oceanography
La Jolla, United States
3 h-index
7 publications
717 citations
Fisheries and Oceans Canada
Ottawa, Canada
3 h-index
7 publications
413 citations
University of Miami
Coral Gables, United States
3 h-index
16 publications
2.4K citations

Ocean University of China
Qingdao, China
3 h-index
8 publications
212 citations
Trent University
Peterborough, Canada
3 h-index
5 publications
574 citations
Tallinn University of Technology
Tallinn, Estonia
3 h-index
7 publications
176 citations
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JGR · 14 publications · 522 citations
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6 publications · 397 citations
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6 publications · 199 citations
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5 publications · 272 citations
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4 publications · 286 citations
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