Two-layer Exchange Flow
Two-Layer Exchange Flow is an estuarine exchange flow model that describes the gravitational circulation in stratified estuaries as a steady, density-driven flow system in which freshwater discharge from rivers forms a seaward-flowing upper layer and denser seawater intrudes landward as a compensating lower layer, distinguished by its simplification of estuarine dynamics into two vertically stacked, counter-advecting layers with sharp interfacial density contrast.
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Publications
2.4K
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108
Authors
57
Institutions
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2017–2026
5
Variants
Two-layer Gravitational Circulation
50
Two-layer hydraulics: a functional approach
Stuart B. Dalziel · Journal of Fluid Mechanics · 1991 · 110 citations
1–5 of 50
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Centre National de la Recherche Scientifique, France
2 publications · 32 citations
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1–5 of 108
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University of British Columbia
Vancouver, Canada
5 h-index
10 publications
254 citations
University of Washington
Seattle, United States
3 h-index
3 publications
113 citations
Woods Hole Oceanographic Institution
Falmouth, United States
3 h-index
5 publications
103 citations

Scripps Institution of Oceanography
La Jolla, United States
3 h-index
5 publications
455 citations
University of Cambridge
Cambridge, United Kingdom
3 h-index
5 publications
180 citations
University of California San Diego
San Diego, United States
3 h-index
6 publications
215 citations
University of Washington Applied Physics Laboratory
Seattle, United States
2 h-index
4 publications
109 citations
Karlsruhe Institute of Technology
Karlsruhe, Germany
2 h-index
3 publications
47 citations
1–8 of 57
13 publications · 632 citations
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9 publications · 503 citations
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4 publications · 123 citations
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4 publications · 98 citations
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2 publications · 56 citations
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