Wind-driven Shelf Circulation
Wind-Driven Shelf Circulation is a large-scale oceanographic circulation pattern on the continental shelf in which the primary driving force is the tangential stress exerted by wind on the sea surface, distinguished by its confinement to shallow, coastal regions and its dynamical balance involving wind forcing, Coriolis effect, and bottom friction.
213
Publications
12.1K
Citations
502
Authors
175
Institutions
Publications per year
2017–2026
20
Parents
213
1–5 of 213
502
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Woods Hole Oceanographic Institution, United States
7 publications · 567 citations
7
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6
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6
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1–5 of 502
175
Oregon State University
Corvallis, United States
19 h-index
53 publications
3.9K citations
Woods Hole Oceanographic Institution
Falmouth, United States
18 h-index
40 publications
3.4K citations

UNSW Sydney
Sydney, Australia
9 h-index
24 publications
1.4K citations
Rutgers, The State University of New Jersey
New Brunswick, United States
9 h-index
21 publications
934 citations

British Oceanographic Data Centre
Liverpool, United Kingdom
7 h-index
16 publications
872 citations

Scripps Institution of Oceanography
La Jolla, United States
6 h-index
30 publications
1.2K citations
University of Washington
Seattle, United States
6 h-index
12 publications
809 citations

Chinese Academy of Sciences
Beijing, China
5 h-index
14 publications
1.3K citations
1–8 of 175
JGR · 50 publications · 3.9K citations
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55 publications · 2.8K citations
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28 publications · 986 citations
19
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9 publications · 460 citations
9
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8 publications · 320 citations
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