Barotropic Instability
Barotropic Instability is a type of hydrodynamic instability arising in a rotating fluid when the horizontal shear of the mean flow violates the Rayleigh criterion, leading to the growth of disturbances in the absence of vertical density stratification.
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428
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2017–2026
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University of California, Los Angeles, United States
11 publications · 847 citations
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University of Reading
Reading, United Kingdom
20 h-index
38 publications
3.2K citations
NOAA Geophysical Fluid Dynamics Laboratory
Princeton, United States
20 h-index
32 publications
1.6K citations
Massachusetts Institute of Technology
Cambridge, United States
19 h-index
29 publications
1.9K citations
Woods Hole Oceanographic Institution
Falmouth, United States
19 h-index
35 publications
1.3K citations

Centre National de la Recherche Scientifique
Paris, France
18 h-index
56 publications
2.3K citations

NSF National Center for Atmospheric Research
Boulder, United States
18 h-index
30 publications
2.2K citations
Princeton University
Princeton, United States
16 h-index
28 publications
1.2K citations
Laboratoire de Météorologie Dynamique
Palaiseau, France
15 h-index
36 publications
1.6K citations
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195 publications · 13.5K citations
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81 publications · 3.4K citations
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JGR · 18 publications · 825 citations
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