Instability of Shear Layers is a hydrodynamic instability phenomenon characterized by the spontaneous growth of perturbations in a fluid flow with a velocity gradient perpendicular to the direction of shear, distinguished from other instabilities by its reliance on continuous vorticity variation across the shear layer in the absence of horizontal temperature gradients.
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2017–2026
38
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Shear Layer Instability
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Centre National de la Recherche Scientifique
Paris, France
13 h-index
23 publications
640 citations
California Institute of Technology
Pasadena, United States
11 h-index
20 publications
1.4K citations
Massachusetts Institute of Technology
Cambridge, United States
11 h-index
15 publications
1.5K citations
University of Minnesota
Minneapolis, United States
9 h-index
20 publications
1.7K citations
Glenn Research Center
Cleveland, United States
9 h-index
13 publications
1.3K citations
University of California, Los Angeles
Los Angeles, United States
8 h-index
25 publications
1.8K citations
University of Cambridge
Cambridge, United Kingdom
8 h-index
12 publications
490 citations
University of California San Diego
San Diego, United States
8 h-index
14 publications
985 citations
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- Journal of Fluid Mechanics
124 publications · 12.1K citations
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- Physics of Fluids
41 publications · 1.6K citations
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- The Physics of Fluids
12 publications · 407 citations
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- AIAA Journal
14 publications · 521 citations
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- Journal of the Atmospheric Sciences
10 publications · 577 citations
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