Barotropic Tides
Barotropic Tides is a tidal dynamics phenomenon characterized by horizontal water motion driven by gravitational forcing, wherein the tidal wave propagates across the ocean surface with minimal vertical shear, distinguishing it from internal (baroclinic) tides by its depth-independent flow structure.
138
Publications
12.3K
Citations
385
Authors
183
Institutions
Publications per year
2017–2026
29
Variants
Barotropic Tide
138
1–5 of 138
385
Laboratoire d’Études en Géophysique et Océanographie Spatiales, France
5 publications · 324 citations
5
h-index
5
h-index
5
h-index
5
h-index
4
h-index
1–5 of 385
183

Stennis Space Center
Bay Saint Louis, United States
9 h-index
27 publications
1.8K citations

Centre National de la Recherche Scientifique
Paris, France
8 h-index
20 publications
745 citations
Laboratoire d’Études en Géophysique et Océanographie Spatiales
Toulouse, France
7 h-index
15 publications
877 citations

Scripps Institution of Oceanography
La Jolla, United States
7 h-index
15 publications
805 citations
Woods Hole Oceanographic Institution
Falmouth, United States
6 h-index
13 publications
687 citations
Oregon State University
Corvallis, United States
6 h-index
10 publications
10.1K citations
University of Michigan
Ann Arbor, United States
5 h-index
8 publications
574 citations
Institut de Recherche pour le Développement
Marseille, France
5 h-index
13 publications
425 citations
1–8 of 183
JGR · 33 publications · 2.2K citations
27
h-index
24 publications · 1.2K citations
21
h-index
14 publications · 620 citations
13
h-index
7 publications · 1.2K citations
7
h-index
7 publications · 482 citations
7
h-index
1–5