Barotropic Flow
Barotropic Flow is a type of fluid flow in atmospheric and oceanic dynamics in which density depends solely on pressure, implying that isopycnals (surfaces of constant density) are parallel to isobars (surfaces of constant pressure), resulting in wind or current velocity that is independent of height or depth.
1.3K
Publications
74.4K
Citations
2.1K
Authors
749
Institutions
Publications per year
2017–2026
112
Variants
Barotropic Fluid Flow
Parents
1.3K
THE DYNAMICS OF LONG WAVES IN A BAROCLINIC WESTERLY CURRENT
J. G. Charney · Journal of Meteorology · 1947 · 1.3K citations · Full text
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Courant Institute of Mathematical Sciences, United States
10 publications · 1.2K citations
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University of California, Los Angeles, United States
10 publications · 623 citations
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749
Massachusetts Institute of Technology
Cambridge, United States
29 h-index
63 publications
4.5K citations
Woods Hole Oceanographic Institution
Falmouth, United States
28 h-index
61 publications
3.7K citations

Scripps Institution of Oceanography
La Jolla, United States
28 h-index
46 publications
3.9K citations
University of California San Diego
San Diego, United States
22 h-index
34 publications
2.9K citations

NSF National Center for Atmospheric Research
Boulder, United States
21 h-index
46 publications
3K citations
NOAA Geophysical Fluid Dynamics Laboratory
Princeton, United States
20 h-index
33 publications
2.5K citations
Princeton University
Princeton, United States
19 h-index
28 publications
2.6K citations
University of Washington
Seattle, United States
19 h-index
38 publications
2.4K citations
1–8 of 749
210 publications · 14.9K citations
63
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199 publications · 11.9K citations
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JGR · 120 publications · 6.6K citations
47
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62 publications · 3.6K citations
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50 publications · 3K citations
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