Equatorial Upwelling
Equatorial Upwelling is an oceanographic phenomenon characterized by the upward movement of cold, nutrient-rich subsurface waters to the surface layer along the equator, driven primarily by the divergence of surface currents due to zonal wind stress and the Coriolis effect.
278
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25K
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711
Authors
266
Institutions
Publications per year
2017–2026
41
278
Ocean Circulation and Tropical Variability in the Coupled Model ECHAM5/MPI-OM
Johann Jungclaus, Noel Keenlyside, M. Botzet et al. · Journal of Climate · 2006 · 909 citations
Amy Clement, Richard Seager, Mark A. Cane et al. · Journal of Climate · 1996 · 618 citations
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NOAA Pacific Marine Environmental Laboratory, United States
7 publications · 450 citations
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266

Centre National de la Recherche Scientifique
Paris, France
15 h-index
42 publications
2.3K citations

University of Hawaiʻi at Mānoa
Honolulu, United States
14 h-index
26 publications
1.7K citations

Scripps Institution of Oceanography
La Jolla, United States
13 h-index
25 publications
1.2K citations

Sorbonne Université
Paris, France
13 h-index
28 publications
1.7K citations
Institut de Recherche pour le Développement
Marseille, France
12 h-index
24 publications
1.1K citations

Christian-Albrechts-Universität zu Kiel
Kiel, Germany
12 h-index
20 publications
1.3K citations
NOAA Pacific Marine Environmental Laboratory
Seattle, United States
12 h-index
17 publications
1K citations

GEOMAR Helmholtz Centre for Ocean Research Kiel
Kiel, Germany
11 h-index
39 publications
1.4K citations
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35 publications · 2K citations
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JGR · 36 publications · 2.2K citations
27
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31 publications · 2.4K citations
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25 publications · 3.5K citations
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13 publications · 1.2K citations
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