Ocean Circulation
Ocean circulation is the large-scale movement of ocean water masses throughout the world's basins, driven by wind stress, internal density gradients, and the Coriolis effect, that functions as the primary mechanism for redistributing heat and carbon globally and regulating Earth's climate.
15.4K
Publications
1.1M
Citations
19.1K
Authors
2.8K
Institutions
Publications per year
2017–2026
2.8K
15.4K
1–5 of 15.4K
19.1K
University of California, Los Angeles, United States
104 publications · 19K citations
56
h-index
51
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49
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49
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45
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1–5 of 19.1K
2.8K
Woods Hole Oceanographic Institution
Falmouth, United States
142 h-index
1.8K publications
157.7K citations

Scripps Institution of Oceanography
La Jolla, United States
119 h-index
1.1K publications
89.9K citations

Centre National de la Recherche Scientifique
Paris, France
116 h-index
2.2K publications
144.1K citations

National Oceanography Centre
Southampton, United Kingdom
102 h-index
1.1K publications
89.6K citations
Massachusetts Institute of Technology
Cambridge, United States
102 h-index
651 publications
69K citations
University of Washington
Seattle, United States
100 h-index
629 publications
65K citations
Oregon State University
Corvallis, United States
97 h-index
670 publications
57.4K citations

Lamont-Doherty Earth Observatory
Sparkill, United States
97 h-index
566 publications
62.7K citations
1–8 of 2.8K
JGR · 2.2K publications · 184.4K citations
187
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2.4K publications · 175.3K citations
177
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1K publications · 68K citations
124
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458 publications · 41.4K citations
106
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1K publications · 46.7K citations
93
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1–5