Breaking Wave Turbulence is a hydrodynamic phenomenon characterized by the chaotic, three-dimensional fluid motion generated during the breaking of surface waves in the nearshore zone, distinguished from other forms of wave-induced turbulence by the abrupt energy dissipation and vortex formation associated with wave collapse and aerated flow structures.
220
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13.7K
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483
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259
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2017–2026
39
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Publications
220
1–5 of 220
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483
- PL
7
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- DT
7
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- KC
6
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- WKW. Kendall Melville
Scripps Institution of Oceanography, United States
6 publications · 1.1K citations
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- IC
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Institutions
259
Centre National de la Recherche Scientifique
Paris, France
14 h-index
28 publications
1.5K citations
Scripps Institution of Oceanography
La Jolla, United States
12 h-index
21 publications
1.7K citations
University of Delaware
Newark, United States
11 h-index
23 publications
1.2K citations
Oregon State University
Corvallis, United States
9 h-index
16 publications
998 citations
National Central University
Taoyuan City, Taiwan
8 h-index
8 publications
334 citations
University of Washington Applied Physics Laboratory
Seattle, United States
7 h-index
18 publications
987 citations
Texas A&M University
College Station, United States
7 h-index
22 publications
681 citations
Cornell University
Ithaca, United States
6 h-index
10 publications
1.1K citations
1–8 of 259
Venues
- Journal of Fluid Mechanics
24 publications · 2.2K citations
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- Coastal Engineering
24 publications · 1.7K citations
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- Journal of Geophysical Research Atmospheres
JGR · 19 publications · 1.8K citations
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- Journal of Physical Oceanography
16 publications · 1.1K citations
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- Journal of Geophysical Research Oceans
15 publications · 632 citations
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