Internal Wave Attenuation
Internal Wave Attenuation is a physical phenomenon in oceanic and atmospheric dynamics whereby the amplitude of internal waves diminishes over time due to energy dissipation mechanisms such as viscous friction, thermal diffusion, and nonlinear wave–wave interactions.
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2.2K
Citations
165
Authors
91
Institutions
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2017–2026
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University of California San Diego
San Diego, United States
5 h-index
9 publications
294 citations

Scripps Institution of Oceanography
La Jolla, United States
4 h-index
8 publications
237 citations
Woods Hole Oceanographic Institution
Falmouth, United States
3 h-index
3 publications
204 citations
Russian Academy of Sciences
Moscow, Russia
3 h-index
4 publications
63 citations

Indian Institute of Technology Roorkee
Roorkee, India
3 h-index
8 publications
98 citations
The University of Tokyo
Tokyo, Japan
2 h-index
6 publications
75 citations

Chinese Academy of Sciences
Beijing, China
2 h-index
10 publications
220 citations

National Sun Yat-sen University
Kaohsiung City, Taiwan
2 h-index
4 publications
85 citations
1–8 of 91
JASA · 4 publications · 254 citations
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4 publications · 150 citations
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3 publications · 233 citations
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3 publications · 128 citations
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JGR · 3 publications · 268 citations
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