Internal Tides
Internal Tides is an oceanic wave phenomenon characterized as a type of internal gravity wave generated when barotropic tidal currents interact with underwater topography, distinguished by its propagation within the stratified interior of the ocean rather than at the surface.
795
Publications
47.6K
Citations
1.3K
Authors
456
Institutions
Publications per year
2017–2026
171
795
Internal Tide Generation in the Deep Ocean
Chris Garrett, Eric Kunze · Annual Review of Fluid Mechanics · 2006 · 739 citations
The Shaping of Continental Slopes by Internal Tides
David A. Cacchione, Lincoln F. Pratson, A. S. Ogston · Science · 2002 · 345 citations
1–5 of 795
1.3K
University of Washington Applied Physics Laboratory, United States
39 publications · 2.9K citations
29
h-index
University of Washington Applied Physics Laboratory, United States
32 publications · 2.2K citations
27
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24
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19
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19
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1–5 of 1.3K
456
University of Washington Applied Physics Laboratory
Seattle, United States
47 h-index
144 publications
12.7K citations

Scripps Institution of Oceanography
La Jolla, United States
45 h-index
155 publications
10.6K citations
University of California San Diego
San Diego, United States
34 h-index
112 publications
7.6K citations
Oregon State University
Corvallis, United States
30 h-index
82 publications
6.1K citations
Woods Hole Oceanographic Institution
Falmouth, United States
27 h-index
90 publications
7K citations

University of Hawaiʻi at Mānoa
Honolulu, United States
26 h-index
78 publications
5.2K citations

Centre National de la Recherche Scientifique
Paris, France
25 h-index
102 publications
4.2K citations
Institute of Oceanology
Qingdao, China
25 h-index
147 publications
5.9K citations
1–8 of 456
193 publications · 14.2K citations
70
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JGR · 103 publications · 7.3K citations
51
h-index
69 publications · 4.3K citations
36
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78 publications · 3.4K citations
35
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26 publications · 1K citations
20
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