Nonlinear Baroclinic Instability
Nonlinear Baroclinic Instability is a theoretical framework in atmospheric and oceanic dynamics that extends the linear theory of baroclinic instability by incorporating finite-amplitude perturbations and nonlinear interactions, thereby capturing the self-sustaining evolution and saturation of large-scale instabilities in stratified, rotating shear flows.
204
Publications
10.3K
Citations
316
Authors
145
Institutions
Publications per year
2017–2026
12
Parents
204
1–5 of 204
316
10
h-index
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145
University of Colorado Boulder
Boulder, United States
9 h-index
11 publications
416 citations
University of Reading
Reading, United Kingdom
9 h-index
15 publications
2.5K citations
Massachusetts Institute of Technology
Cambridge, United States
9 h-index
12 publications
408 citations
Woods Hole Oceanographic Institution
Falmouth, United States
8 h-index
9 publications
490 citations
University of Oxford
Oxford, United Kingdom
7 h-index
19 publications
491 citations

Centre National de la Recherche Scientifique
Paris, France
6 h-index
15 publications
529 citations
NOAA Geophysical Fluid Dynamics Laboratory
Princeton, United States
6 h-index
8 publications
494 citations

NSF National Center for Atmospheric Research
Boulder, United States
6 h-index
13 publications
500 citations
1–8 of 145
62 publications · 4.2K citations
28
h-index
23 publications · 1.3K citations
15
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15 publications · 440 citations
13
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JGR · 11 publications · 559 citations
11
h-index
11 publications · 820 citations
10
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1–5