Internal Wave Breaking
Internal Wave Breaking is a physical process in stratified fluid dynamics wherein internal waves, propagating through density gradients in fluids such as the ocean or atmosphere, become unstable and dissipate their energy via turbulence, thereby enabling diapycnal mixing through the irreversible transfer of wave energy into small-scale shear-driven turbulent motions.
163
Publications
9.6K
Citations
378
Authors
190
Institutions
Publications per year
2017–2026
32
163
1–5 of 163
378
8
h-index
Laboratoire des Écoulements Géophysiques et Industriels, France
5 publications · 489 citations
5
h-index
5
h-index
Royal Netherlands Institute for Sea Research, Netherlands
5 publications · 103 citations
5
h-index
NOAA Geophysical Fluid Dynamics Laboratory, United States
5 publications · 316 citations
5
h-index
1–5 of 378
190
Woods Hole Oceanographic Institution
Falmouth, United States
13 h-index
21 publications
2.7K citations

Scripps Institution of Oceanography
La Jolla, United States
9 h-index
17 publications
1.1K citations

The University of Western Australia
Perth, Australia
8 h-index
11 publications
781 citations

University of Oslo
Oslo, Norway
5 h-index
13 publications
1.2K citations
Royal Netherlands Institute for Sea Research
Den Burg, The Netherlands
5 h-index
10 publications
198 citations
Stanford University
Stanford, United States
5 h-index
11 publications
598 citations
University of Southampton
Southampton, United Kingdom
5 h-index
14 publications
610 citations

Centre National de la Recherche Scientifique
Paris, France
5 h-index
10 publications
694 citations
1–8 of 190
33 publications · 2.5K citations
26
h-index
13 publications · 1.6K citations
13
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JGR · 14 publications · 932 citations
13
h-index
7 publications · 228 citations
7
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7 publications · 300 citations
7
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1–5