Wind-driven Equatorial Circulation
Wind-Driven Equatorial Circulation is a theoretical framework within equatorial oceanography that describes the large-scale, wind-forced movement of surface and subsurface waters along the equatorial band, distinguished by its dependence on zonal wind stress and the resulting dynamical balance involving the Coriolis effect and pressure gradients.
92
Publications
5.6K
Citations
233
Authors
117
Institutions
Publications per year
2017–2026
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117

Centre National de la Recherche Scientifique
Paris, France
5 h-index
12 publications
600 citations

University of Hawaiʻi at Mānoa
Honolulu, United States
4 h-index
8 publications
885 citations
University of Washington
Seattle, United States
4 h-index
7 publications
243 citations

Instituto Nacional de Pesquisas Espaciais
São José dos Campos, Brazil
4 h-index
11 publications
334 citations
California Institute of Technology
Pasadena, United States
3 h-index
4 publications
203 citations

NSF National Center for Atmospheric Research
Boulder, United States
3 h-index
4 publications
241 citations
University of Wisconsin–Madison
Madison, United States
3 h-index
5 publications
206 citations
Institut de Recherche pour le Développement
Marseille, France
3 h-index
11 publications
497 citations
1–8 of 117
17 publications · 1.4K citations
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JGR · 10 publications · 693 citations
10
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5 publications · 219 citations
5
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5 publications · 209 citations
5
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4 publications · 390 citations
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