Wind-driven Circulation Variability
Wind-Driven Circulation Variability is a dynamic oceanographic phenomenon within the broader class of ocean circulation variability, distinguished by its primary dependence on temporal fluctuations in wind stress forcing over the sea surface, which modulate the strength and structure of large-scale gyres, western boundary currents, and Ekman transport systems.
269
Publications
15.9K
Citations
692
Authors
272
Institutions
Publications per year
2017–2026
26
269
1–5 of 269
692
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Massachusetts Institute of Technology, United States
4 publications · 170 citations
4
h-index
GEOMAR Helmholtz Centre for Ocean Research Kiel, Germany
4 publications · 564 citations
4
h-index
1–5 of 692
272
University of Miami
Coral Gables, United States
13 h-index
27 publications
1.9K citations

Centre National de la Recherche Scientifique
Paris, France
12 h-index
28 publications
1.4K citations
Woods Hole Oceanographic Institution
Falmouth, United States
10 h-index
16 publications
544 citations
Rutgers, The State University of New Jersey
New Brunswick, United States
9 h-index
20 publications
1.1K citations

British Oceanographic Data Centre
Liverpool, United Kingdom
8 h-index
18 publications
1.1K citations

University of Hawaiʻi at Mānoa
Honolulu, United States
7 h-index
10 publications
2.3K citations

Scripps Institution of Oceanography
La Jolla, United States
7 h-index
13 publications
499 citations
Institut de Recherche pour le Développement
Marseille, France
7 h-index
14 publications
521 citations
1–8 of 272
JGR · 51 publications · 4.4K citations
39
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51 publications · 2.3K citations
29
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16 publications · 519 citations
14
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12 publications · 608 citations
12
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11 publications · 361 citations
11
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