Oceanic Ekman Layer
Oceanic Ekman Layer is a theoretical boundary layer in geophysical fluid dynamics that describes the vertical structure of wind-driven ocean currents in the upper ocean, distinguished by a balance between the Coriolis force, vertical eddy viscosity, and applied wind stress, resulting in a characteristic spiral of current velocity with depth.
145
Publications
8K
Citations
337
Authors
145
Institutions
Publications per year
2017–2026
16
Parents
145
Sonia T. Bauer, Gary L. Hitchcock, Donald B. Olson · Deep Sea Research Part A Oceanographic Research Papers · 1991 · 261 citations
1–5 of 145
337
NOAA Geophysical Fluid Dynamics Laboratory, United States
3 publications · 99 citations
3
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3
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University of California, Los Angeles, United States
3 publications · 212 citations
3
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3
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3
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1–5 of 337
145
Woods Hole Oceanographic Institution
Falmouth, United States
9 h-index
12 publications
1.3K citations
University of California San Diego
San Diego, United States
7 h-index
12 publications
527 citations

Scripps Institution of Oceanography
La Jolla, United States
6 h-index
10 publications
379 citations
Florida State University
Tallahassee, United States
6 h-index
11 publications
532 citations
Massachusetts Institute of Technology
Cambridge, United States
5 h-index
7 publications
506 citations
University of Washington
Seattle, United States
4 h-index
5 publications
356 citations
Institute of Oceanology
Qingdao, China
3 h-index
6 publications
314 citations

Naval Postgraduate School
Monterey, United States
3 h-index
5 publications
267 citations
1–8 of 145
37 publications · 2.1K citations
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JGR · 16 publications · 774 citations
15
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9 publications · 436 citations
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5 publications · 89 citations
6
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4 publications · 143 citations
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