Internal Tide Nonlinearity
Internal Tide Nonlinearity is a geophysical phenomenon characterized by the deviation from linear wave theory in the propagation and interaction of internal tides, arising from finite-amplitude dynamics and nonlinear coupling between oceanic density stratification and tidal forcing.
57
Publications
4.6K
Citations
143
Authors
71
Institutions
Publications per year
2017–2026
12
Parents
57
1–5 of 57
143
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Woods Hole Oceanographic Institution, United States
3 publications · 518 citations
3
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3
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1–5 of 143
71
Woods Hole Oceanographic Institution
Falmouth, United States
8 h-index
21 publications
2.5K citations
Royal Netherlands Institute for Sea Research
Den Burg, The Netherlands
6 h-index
9 publications
469 citations
Institute of Oceanology
Qingdao, China
4 h-index
10 publications
287 citations

Naval Postgraduate School
Monterey, United States
4 h-index
9 publications
961 citations

Chinese Academy of Sciences
Beijing, China
4 h-index
8 publications
253 citations

Scripps Institution of Oceanography
La Jolla, United States
3 h-index
3 publications
294 citations

Monterey Bay Aquarium Research Institute
Castroville, United States
3 h-index
3 publications
483 citations
South China Sea Institute Of Oceanology
Guangzhou, China
3 h-index
10 publications
287 citations
1–8 of 71
15 publications · 1.9K citations
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JGR · 9 publications · 859 citations
9
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8 publications · 401 citations
8
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6 publications · 319 citations
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6 publications · 222 citations
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