Barotropic Circulation
Barotropic Circulation is a type of ocean circulation characterized by horizontal flow that is depth-independent, in which pressure gradients arise solely from variations in sea surface height and the resultant currents are uniform throughout the water column.
298
Publications
18.1K
Citations
725
Authors
282
Institutions
Publications per year
2017–2026
26
Variants
Barotropic Flow
298
Finlo Cottier, Vigdis Tverberg, Mark Inall et al. · Journal of Geophysical Research Atmospheres · 2005 · 491 citations · Full text
1–5 of 298
725
6
h-index
4
h-index
4
h-index
4
h-index
4
h-index
1–5 of 725
282
Woods Hole Oceanographic Institution
Falmouth, United States
19 h-index
34 publications
1.6K citations

Scripps Institution of Oceanography
La Jolla, United States
11 h-index
14 publications
1K citations
Massachusetts Institute of Technology
Cambridge, United States
11 h-index
17 publications
911 citations
Japan Agency for Marine-Earth Science and Technology
Yokosuka, Japan
8 h-index
20 publications
582 citations

Centre National de la Recherche Scientifique
Paris, France
8 h-index
15 publications
887 citations
Oregon State University
Corvallis, United States
7 h-index
13 publications
687 citations
Planetary Science Institute
Tucson, United States
7 h-index
13 publications
643 citations
Ifremer
Brest, France
7 h-index
9 publications
427 citations
1–8 of 282
95 publications · 6.1K citations
45
h-index
JGR · 47 publications · 3.5K citations
31
h-index
20 publications · 1K citations
16
h-index
11 publications · 554 citations
11
h-index
13 publications · 420 citations
11
h-index
1–5