Stratified Shear Flows
Stratified Shear Flows is a fluid dynamical phenomenon characterized by the presence of density stratification interacting with velocity gradients, where the stabilizing effect of buoyancy competes with the destabilizing effect of shear, leading to complex turbulence and mixing processes in geophysical and engineering flows.
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University of Cambridge
Cambridge, United Kingdom
21 h-index
56 publications
2.3K citations
Oregon State University
Corvallis, United States
18 h-index
33 publications
1.7K citations
University of California San Diego
San Diego, United States
18 h-index
45 publications
2.4K citations

University of Toronto
Toronto, Canada
18 h-index
36 publications
2K citations

Centre National de la Recherche Scientifique
Paris, France
17 h-index
34 publications
1.2K citations
Massachusetts Institute of Technology
Cambridge, United States
14 h-index
24 publications
1.3K citations
Arizona State University
Tempe, United States
12 h-index
25 publications
1.4K citations

Tel Aviv University
Tel Aviv, Israel
10 h-index
32 publications
1.3K citations
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135 publications · 11.3K citations
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