Zonal Flow Instability is a theoretical construct in atmospheric and oceanic dynamics that characterizes the propensity of a zonally symmetric, barotropic flow to develop perturbations and transition into unstable, wave-like motions due to meridional gradients in potential vorticity.
361
Publications
17K
Citations
808
Authors
261
Institutions
Publications per year
2017–2026
40
Parents
Publications
361
1–5 of 361
Authors
808
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17
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9
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8
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7
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1–5 of 808
Institutions
261
University of California San Diego
San Diego, United States
19 h-index
63 publications
4.6K citations
Massachusetts Institute of Technology
Cambridge, United States
17 h-index
26 publications
2.6K citations
Princeton Plasma Physics Laboratory
Princeton, United States
12 h-index
26 publications
1.9K citations
National Institute for Fusion Science
Toki, Japan
12 h-index
46 publications
1.4K citations
University of California, Los Angeles
Los Angeles, United States
11 h-index
26 publications
2.3K citations
Kyoto University
Kyoto, Japan
11 h-index
24 publications
687 citations
Woods Hole Oceanographic Institution
Falmouth, United States
10 h-index
17 publications
634 citations
Princeton University
Princeton, United States
10 h-index
18 publications
1.4K citations
1–8 of 261
Venues
- Journal of the Atmospheric Sciences
89 publications · 5.8K citations
35
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- Physics of Plasmas
53 publications · 2.1K citations
26
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- Journal of Fluid Mechanics
28 publications · 1.3K citations
22
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- Journal of Physical Oceanography
21 publications · 771 citations
16
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- Nuclear Fusion
18 publications · 701 citations
14
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