Baroclinic Tides
Baroclinic Tides is a tidal phenomenon within the broader category of internal tides, distinguished by the generation of vertically stratified, density-dependent currents due to the deformation of tidal waves across density gradients in a baroclinic ocean.
219
Publications
12.1K
Citations
521
Authors
195
Institutions
Publications per year
2017–2026
34
219
1–5 of 219
521
8
h-index
7
h-index
7
h-index
7
h-index
6
h-index
1–5 of 521
195

Scripps Institution of Oceanography
La Jolla, United States
16 h-index
38 publications
2.9K citations

University of Hawaiʻi at Mānoa
Honolulu, United States
12 h-index
32 publications
2.2K citations
University of California San Diego
San Diego, United States
12 h-index
27 publications
1.2K citations
University of Washington Applied Physics Laboratory
Seattle, United States
11 h-index
22 publications
1.8K citations
Oregon State University
Corvallis, United States
11 h-index
17 publications
898 citations
Fisheries and Oceans Canada
Ottawa, Canada
9 h-index
19 publications
1.2K citations
Institute of Oceanology
Qingdao, China
7 h-index
33 publications
1.7K citations
Woods Hole Oceanographic Institution
Falmouth, United States
7 h-index
18 publications
660 citations
1–8 of 195
54 publications · 3.4K citations
35
h-index
JGR · 41 publications · 2.3K citations
27
h-index
26 publications · 1.2K citations
21
h-index
17 publications · 1.2K citations
15
h-index
5 publications · 210 citations
5
h-index
1–5