Internal Tide Variability
Internal Tide Variability is a geophysical phenomenon characterized by temporal and spatial fluctuations in the amplitude, phase, and propagation of internal tides due to interactions with background oceanographic conditions, topographic features, and mesoscale flow dynamics.
223
Publications
11K
Citations
525
Authors
223
Institutions
Publications per year
2017–2026
57
Parents
223
1–5 of 223
525
University of Washington Applied Physics Laboratory, United States
15 publications · 1K citations
15
h-index
University of Washington Applied Physics Laboratory, United States
11 publications · 864 citations
11
h-index
7
h-index
7
h-index
6
h-index
1–5 of 525
223
University of Washington Applied Physics Laboratory
Seattle, United States
21 h-index
37 publications
2.3K citations

Scripps Institution of Oceanography
La Jolla, United States
16 h-index
33 publications
1.8K citations
Institute of Oceanology
Qingdao, China
14 h-index
63 publications
2.7K citations

Ocean University of China
Qingdao, China
12 h-index
41 publications
1.7K citations

Chinese Academy of Sciences
Beijing, China
12 h-index
49 publications
2.4K citations

University of Hawaiʻi at Mānoa
Honolulu, United States
12 h-index
29 publications
1.2K citations
University of California San Diego
San Diego, United States
11 h-index
22 publications
1.1K citations
Oregon State University
Corvallis, United States
11 h-index
32 publications
2.3K citations
1–8 of 223
42 publications · 2.9K citations
33
h-index
23 publications · 1.3K citations
21
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JGR · 26 publications · 1.3K citations
20
h-index
12 publications · 922 citations
11
h-index
11 publications · 588 citations
11
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1–5