Geostrophic Flow
Geostrophic Flow is a steady oceanic flow in which the pressure gradient force is balanced by the Coriolis force, resulting in motion parallel to the isobars.
2.9K
Publications
170.6K
Citations
5.3K
Authors
1.3K
Institutions
Publications per year
2017–2026
280
2.9K
1–5 of 2.9K
5.3K
University of California, Los Angeles, United States
24 publications · 2.4K citations
22
h-index
15
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15
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14
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13
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1–5 of 5.3K
1.3K
Woods Hole Oceanographic Institution
Falmouth, United States
48 h-index
171 publications
9.7K citations

Centre National de la Recherche Scientifique
Paris, France
47 h-index
308 publications
21.8K citations

NSF National Center for Atmospheric Research
Boulder, United States
38 h-index
95 publications
7.9K citations

Scripps Institution of Oceanography
La Jolla, United States
38 h-index
108 publications
9.5K citations
Massachusetts Institute of Technology
Cambridge, United States
36 h-index
77 publications
6.9K citations
University of Washington
Seattle, United States
34 h-index
96 publications
7.5K citations
University of Reading
Reading, United Kingdom
25 h-index
71 publications
6.4K citations
University of Miami
Coral Gables, United States
24 h-index
61 publications
4K citations
1–8 of 1.3K
335 publications · 20.2K citations
75
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JGR · 245 publications · 16.9K citations
71
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196 publications · 15.4K citations
63
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173 publications · 8.7K citations
57
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84 publications · 3.6K citations
37
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1–5