Two-layer Circulation
Two-Layer Circulation is a hydrodynamic model in estuarine stratification that describes the gravitational circulation characterized by a net outflow of buoyant freshwater in the upper layer and a compensating inflow of denser saline water in the lower layer, driven by longitudinal density gradients.
130
Publications
6.6K
Citations
309
Authors
127
Institutions
Publications per year
2017–2026
12
Parents
130
ON THE WIND-DRIVEN OCEAN CIRCULATION
Walter Munk · Journal of Meteorology · 1950 · 944 citations · Full text
Stratified coastal ocean interactions with tropical cyclones
Scott Glenn, Travis Miles, Gregory Seroka et al. · Nature Communications · 2016 · 215 citations · Full text
1–5 of 130
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Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques, France
4 publications · 195 citations
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3
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1–5 of 309
127

University of Alberta
Edmonton, Canada
8 h-index
19 publications
438 citations
University of California San Diego
San Diego, United States
7 h-index
13 publications
623 citations

Scripps Institution of Oceanography
La Jolla, United States
6 h-index
10 publications
1.3K citations
Woods Hole Oceanographic Institution
Falmouth, United States
6 h-index
6 publications
508 citations

University of Limerick
Limerick, Ireland
4 h-index
4 publications
112 citations
The University of Tokyo
Tokyo, Japan
3 h-index
3 publications
92 citations
University of Cambridge
Cambridge, United Kingdom
3 h-index
5 publications
206 citations

Centre National de la Recherche Scientifique
Paris, France
3 h-index
8 publications
198 citations
1–8 of 127
36 publications · 1.7K citations
24
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19 publications · 698 citations
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7 publications · 384 citations
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5 publications · 210 citations
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3 publications · 74 citations
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1–5