Nonlinear Barotropic Instability is a dynamical fluid instability mechanism within atmospheric and oceanic flows characterized by the finite-amplitude growth and evolution of disturbances in a barotropic fluid, where nonlinear advection processes fundamentally alter the stability properties and long-term behavior of the flow beyond the predictions of linear theory.
64
Publications
3.5K
Citations
130
Authors
79
Institutions
Publications per year
2017–2026
4
Parents
Publications
64
1–5 of 64
Authors
130
- VZ
4
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- XC
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- PL
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- TA
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1–5 of 130
Institutions
79
Laboratoire de Météorologie Dynamique
Palaiseau, France
4 h-index
9 publications
923 citations
Colorado State University
Fort Collins, United States
3 h-index
10 publications
3.5K citations
Sorbonne Université
Paris, France
3 h-index
6 publications
369 citations
Scripps Institution of Oceanography
La Jolla, United States
3 h-index
3 publications
321 citations
University of California San Diego
San Diego, United States
3 h-index
3 publications
260 citations
University of Oxford
Oxford, United Kingdom
3 h-index
7 publications
184 citations
Institute of Atmospheric Physics
Beijing, China
3 h-index
8 publications
126 citations
Centre National de la Recherche Scientifique
Paris, France
2 h-index
4 publications
256 citations
1–8 of 79
Venues
- Journal of the Atmospheric Sciences
18 publications · 1.4K citations
16
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- Journal of Fluid Mechanics
12 publications · 786 citations
11
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- Journal of Physical Oceanography
7 publications · 177 citations
7
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- Tellus A Dynamic Meteorology and Oceanography
4 publications · 449 citations
4
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- Geophysical & Astrophysical Fluid Dynamics
3 publications · 63 citations
3
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1–5