Equatorial Countercurrent
An Equatorial Countercurrent is a surface oceanic current that flows eastward between the northward and southward-flowing equatorial currents, driven by the convergence of trade winds and the resulting meridional piling of water west of the Atlantic, Indian, and Pacific Ocean basins.
222
Publications
12.5K
Citations
452
Authors
153
Institutions
Publications per year
2017–2026
19
Variants
Equatorial Counter-current
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Jérôme Vialard, Christophe Menkès, Jean‐Philippe Boulanger et al. · Journal of Physical Oceanography · 2001 · 228 citations · Full text
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NOAA Atlantic Oceanographic and Meteorological Laboratories, United States
8 publications · 498 citations
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7
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NOAA Atlantic Oceanographic and Meteorological Laboratories, United States
7 publications · 353 citations
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Institute of Oceanology
Qingdao, China
16 h-index
73 publications
2K citations

University of Hawaiʻi at Mānoa
Honolulu, United States
15 h-index
29 publications
2.2K citations

Chinese Academy of Sciences
Beijing, China
13 h-index
57 publications
1.7K citations
University of Chinese Academy of Sciences
Beijing, China
13 h-index
34 publications
919 citations
NOAA Pacific Marine Environmental Laboratory
Seattle, United States
11 h-index
15 publications
1.4K citations

Scripps Institution of Oceanography
La Jolla, United States
9 h-index
14 publications
752 citations
University of Miami
Coral Gables, United States
8 h-index
14 publications
546 citations

University of Hawaii System
Honolulu, United States
8 h-index
14 publications
1.2K citations
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JGR · 75 publications · 5.1K citations
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56 publications · 4K citations
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16 publications · 567 citations
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10 publications · 350 citations
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7 publications · 224 citations
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