Two-layer Flow Structure
Two-Layer Flow Structure is a hydrodynamic configuration in estuarine systems characterized by the stratification of water into two distinct vertical layers—typically a fresher, faster-moving upper layer and a denser, slower-moving lower layer—driven by salinity and density gradients, which governs the exchange of momentum, salt, and nutrients in partially mixed and highly stratified estuaries.
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Nelson G. Hogg, Henry Stommel · Proceedings of the Royal Society of London A Mathematical and Physical Sciences · 1985 · 205 citations
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Woods Hole Oceanographic Institution
Falmouth, United States
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19 publications
1.2K citations

Centre National de la Recherche Scientifique
Paris, France
10 h-index
24 publications
663 citations

Scripps Institution of Oceanography
La Jolla, United States
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13 publications
1K citations
University of California San Diego
San Diego, United States
7 h-index
9 publications
351 citations

Perm State University
Perm, Russia
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12 publications
370 citations
Massachusetts Institute of Technology
Cambridge, United States
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9 publications
566 citations
Virginia Tech
Blacksburg, United States
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13 publications
671 citations
University of Washington
Seattle, United States
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6 publications
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