Wind-driven Coastal Circulation
Wind-Driven Coastal Circulation is a coastal circulation pattern, distinguished from other such patterns by its primary generation through the direct action of wind stress on the ocean surface along continental margins, resulting in spatially organized flow structures such as coastal upwelling, downwelling, and alongshore currents.
107
Publications
5.5K
Citations
289
Authors
128
Institutions
Publications per year
2017–2026
11
Parents
107
1–5 of 107
289
4
h-index
3
h-index
University of Maryland Center for Environmental Science, United States
3 publications · 374 citations
3
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3
h-index
University of California, Los Angeles, United States
1 publications · 15 citations
2
h-index
1–5 of 289
128
Woods Hole Oceanographic Institution
Falmouth, United States
9 h-index
12 publications
631 citations

Centro de Investigación Científica y de Educación Superior de Ensenada
Ensenada, Mexico
5 h-index
7 publications
334 citations
Oregon State University
Corvallis, United States
5 h-index
9 publications
526 citations

Scripps Institution of Oceanography
La Jolla, United States
5 h-index
12 publications
583 citations

Plymouth Marine Laboratory
Plymouth, United Kingdom
3 h-index
3 publications
136 citations
University of Delaware
Newark, United States
3 h-index
6 publications
564 citations
University of California San Diego
San Diego, United States
3 h-index
3 publications
143 citations
The University of Tokyo
Tokyo, Japan
3 h-index
7 publications
451 citations
1–8 of 128
20 publications · 1.1K citations
15
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13 publications · 953 citations
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JGR · 14 publications · 1.1K citations
12
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6 publications · 124 citations
6
h-index
3 publications · 109 citations
3
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