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

Authors

309

  1. MC
    Michel Crépon

    Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques, France

    4 publications · 195 citations

    4

    h-index

  2. ES
    E. S. Benilov

    University of Limerick, Ireland

    4 publications · 112 citations

    4

    h-index

  3. BS
    Bruce Sutherland

    University of Alberta, Canada

    3 publications · 94 citations

    3

    h-index

  4. MR
    M. R. Flynn

    University of Alberta, Canada

    3 publications · 86 citations

    3

    h-index

  5. PF
    P. F. Linden

    University of Cambridge, United Kingdom

    3 publications · 145 citations

    3

    h-index

1–5 of 309

Venues

  1. Journal of Physical Oceanography

    36 publications · 1.7K citations

    24

    h-index

  2. Journal of Fluid Mechanics

    19 publications · 698 citations

    16

    h-index

  3. Journal of the Atmospheric Sciences

    7 publications · 384 citations

    7

    h-index

  4. Tellus A Dynamic Meteorology and Oceanography

    5 publications · 210 citations

    5

    h-index

  5. Physics of Fluids

    3 publications · 74 citations

    3

    h-index

1–5