Linear Barotropic Instability
Linear Barotropic Instability is a theoretical framework in geophysical fluid dynamics that characterizes the inherent instability of large-scale atmospheric or oceanic flows on a beta plane under the assumption of no vertical shear, where perturbations grow exponentially due to the interaction between the meridional gradient of the background vorticity and the wave-like disturbances constrained to a single vertical mode.
65
Publications
2.6K
Citations
127
Authors
78
Institutions
Publications per year
2017–2026
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1–5 of 65
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University of California, Los Angeles, United States
3 publications · 276 citations
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2
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1–5 of 127
78

NSF National Center for Atmospheric Research
Boulder, United States
3 h-index
5 publications
500 citations
NOAA Geophysical Fluid Dynamics Laboratory
Princeton, United States
3 h-index
5 publications
165 citations
Woods Hole Oceanographic Institution
Falmouth, United States
3 h-index
7 publications
216 citations

University of Hawaiʻi at Mānoa
Honolulu, United States
2 h-index
2 publications
110 citations
Institute of Oceanology. PP Shirshov Russian Academy of Sciences
Moscow, Russia
2 h-index
3 publications
168 citations
University of Cambridge
Cambridge, United Kingdom
2 h-index
2 publications
30 citations

University of KwaZulu-Natal
Durban, South Africa
2 h-index
4 publications
57 citations
University of California, Los Angeles
Los Angeles, United States
2 h-index
5 publications
148 citations
1–8 of 78
23 publications · 861 citations
18
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8 publications · 274 citations
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6 publications · 201 citations
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2 publications · 57 citations
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2 publications · 158 citations
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