Internal Tide Scattering
Internal Tide Scattering is the phenomenon in physical oceanography whereby internal tides, after generation, undergo spatial and directional dispersion due to interactions with complex topography or background stratification, distinguishing it from coherent internal tide propagation by introducing incoherent, higher-wavenumber components into the internal wave field.
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Publications
1.3K
Citations
75
Authors
52
Institutions
Publications per year
2017–2026
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Massachusetts Institute of Technology
Cambridge, United States
5 h-index
5 publications
345 citations
Oregon State University
Corvallis, United States
3 h-index
3 publications
244 citations

University of Hawaii System
Honolulu, United States
2 h-index
4 publications
298 citations
South China Sea Institute Of Oceanology
Guangzhou, China
2 h-index
4 publications
85 citations
Qingdao National Laboratory for Marine Science and Technology
Qingdao, China
2 h-index
8 publications
104 citations

Scripps Institution of Oceanography
La Jolla, United States
2 h-index
2 publications
115 citations

Ocean University of China
Qingdao, China
2 h-index
10 publications
130 citations
Polar Research Institute of China
Shanghai, China
2 h-index
2 publications
26 citations
1–8 of 52
5 publications · 254 citations
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3 publications · 209 citations
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JGR · 2 publications · 149 citations
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2 publications · 29 citations
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2 publications · 196 citations
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