Geostrophic Circulation
Geostrophic Circulation is a theoretical construct in large-scale ocean circulation that describes a steady, horizontal flow of seawater in which the Coriolis force balances the horizontal pressure gradient force, arising from density variations and enabling the inference of ocean currents from hydrographic data.
913
Publications
65.5K
Citations
2K
Authors
548
Institutions
Publications per year
2017–2026
99
913
Circulation in the Western Mediterranean Sea
Claude Millot · Journal of Marine Systems · 1999 · 1.4K citations
1–5 of 913
2K
13
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9
h-index
NOAA Atlantic Oceanographic and Meteorological Laboratories, United States
8 publications · 625 citations
8
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8
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8
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1–5 of 2K
548
Woods Hole Oceanographic Institution
Falmouth, United States
34 h-index
87 publications
6K citations

Scripps Institution of Oceanography
La Jolla, United States
31 h-index
78 publications
7.3K citations

Centre National de la Recherche Scientifique
Paris, France
23 h-index
80 publications
6.6K citations
University of California San Diego
San Diego, United States
20 h-index
48 publications
2.9K citations

National Oceanography Centre
Southampton, United Kingdom
18 h-index
44 publications
2.5K citations
Massachusetts Institute of Technology
Cambridge, United States
17 h-index
26 publications
4.5K citations
University of Miami
Coral Gables, United States
16 h-index
26 publications
1.5K citations
NOAA Pacific Marine Environmental Laboratory
Seattle, United States
16 h-index
24 publications
1K citations
1–8 of 548
JGR · 126 publications · 11.3K citations
57
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152 publications · 10.3K citations
54
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29 publications · 3.5K citations
26
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35 publications · 1.5K citations
24
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30 publications · 2.1K citations
24
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1–5