Barotropic Dynamics
Barotropic Dynamics is a theoretical framework in geophysical fluid dynamics that describes the large-scale motion of fluids in which density depends only on pressure, leading to depth-independent horizontal flow driven by gradients in the free surface and modulated by the Coriolis effect.
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2017–2026
110
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Numerical Integration of the Barotropic Vorticity Equation
J. G. Charney, John von Neumann · Tellus · 1950 · 704 citations · Full text
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NOAA Geophysical Fluid Dynamics Laboratory, United States
9 publications · 777 citations
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University of California, Los Angeles, United States
8 publications · 740 citations
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NSF National Center for Atmospheric Research
Boulder, United States
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43 publications
4.4K citations

Scripps Institution of Oceanography
La Jolla, United States
23 h-index
43 publications
3.1K citations
Woods Hole Oceanographic Institution
Falmouth, United States
23 h-index
42 publications
3.1K citations
NOAA Geophysical Fluid Dynamics Laboratory
Princeton, United States
21 h-index
44 publications
3.2K citations
Massachusetts Institute of Technology
Cambridge, United States
20 h-index
39 publications
3.4K citations
Princeton University
Princeton, United States
19 h-index
34 publications
2.1K citations
University of Washington
Seattle, United States
18 h-index
34 publications
4.5K citations

Centre National de la Recherche Scientifique
Paris, France
18 h-index
52 publications
2.6K citations
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168 publications · 11.3K citations
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150 publications · 9.2K citations
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JGR · 80 publications · 5.2K citations
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39 publications · 2.6K citations
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41 publications · 1.8K citations
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