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.

305

Publications

12K

Citations

691

Authors

330

Institutions

Publications per year

2017–2026

47

Authors

691

  1. IS
    Ilya Simanovskii

    Technion – Israel Institute of Technology, Israel

    6 publications · 193 citations

    6

    h-index

  2. GA
    Gregory A. Lawrence

    University of British Columbia, Canada

    5 publications · 273 citations

    5

    h-index

  3. YR
    Yuriko Renardy

    Virginia Tech, United States

    5 publications · 253 citations

    5

    h-index

  4. JP
    Joseph Pedlosky

    Woods Hole Oceanographic Institution, United States

    4 publications · 414 citations

    4

    h-index

  5. CP
    C. Pozrikidis

    University of California San Diego, United States

    4 publications · 139 citations

    4

    h-index

1–5 of 691

Venues

  1. Journal of Fluid Mechanics

    37 publications · 2.2K citations

    25

    h-index

  2. Journal of Physical Oceanography

    31 publications · 1.1K citations

    20

    h-index

  3. Journal of the Atmospheric Sciences

    16 publications · 1.1K citations

    12

    h-index

  4. Physics of Fluids

    12 publications · 343 citations

    12

    h-index

  5. Tellus A Dynamic Meteorology and Oceanography

    9 publications · 355 citations

    9

    h-index

1–5