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.

50

Publications

2.4K

Citations

108

Authors

57

Institutions

Publications per year

2017–2026

5

Variants

Two-layer Gravitational Circulation

Authors

108

  1. GA
    Gregory A. Lawrence

    University of British Columbia, Canada

    4 publications · 89 citations

    4

    h-index

  2. RP
    Roger Pieters

    University of British Columbia, Canada

    2 publications · 55 citations

    2

    h-index

  3. ME
    Maria Eletta Negretti

    Centre National de la Recherche Scientifique, France

    2 publications · 32 citations

    2

    h-index

  4. GH
    Gerhard H. Jirka

    Karlsruhe Institute of Technology, Germany

    2 publications · 32 citations

    2

    h-index

  5. LA
    Laurence Armi

    Scripps Institution of Oceanography, United States

    2 publications · 270 citations

    2

    h-index

1–5 of 108

Venues

  1. Journal of Physical Oceanography

    13 publications · 632 citations

    13

    h-index

  2. Journal of Fluid Mechanics

    9 publications · 503 citations

    9

    h-index

  3. Geophysical Research Letters

    4 publications · 123 citations

    4

    h-index

  4. Journal of Hydraulic Research

    4 publications · 98 citations

    4

    h-index

  5. Geophysical & Astrophysical Fluid Dynamics

    2 publications · 56 citations

    2

    h-index

1–5