Estuarine Circulation

Estuarine Circulation is a hydrodynamic process characterized by the gravitational circulation and density-driven flow structure in estuaries, where freshwater from rivers moves seaward over a deeper, landward-flowing layer of denser seawater, driven primarily by the longitudinal salinity gradient and modulated by tidal mixing, bathymetry, and Earth's rotation.

999

Publications

56.5K

Citations

2.3K

Authors

750

Institutions

Publications per year

2017–2026

163

Authors

2.3K

  1. AV
    Arnoldo Valle‐Levinson

    University of Florida, United States

    31 publications · 1.4K citations

    23

    h-index

  2. HB
    Hans Burchard

    Leibniz Institute for Baltic Sea Research Warnemünde, Germany

    17 publications · 1.1K citations

    16

    h-index

  3. CL
    Chunyan Li

    Louisiana State University, United States

    16 publications · 645 citations

    15

    h-index

  4. WR
    W. Rockwell Geyer

    Woods Hole Oceanographic Institution, United States

    14 publications · 2.1K citations

    13

    h-index

  5. ML
    Ming Li

    University of Maryland Center for Environmental Science, United States

    12 publications · 620 citations

    12

    h-index

1–5 of 2.3K

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 89 publications · 6.4K citations

    49

    h-index

  2. Estuarine Coastal and Shelf Science

    121 publications · 6.3K citations

    47

    h-index

  3. Journal of Physical Oceanography

    63 publications · 4.2K citations

    36

    h-index

  4. Journal of Geophysical Research Oceans

    46 publications · 2.2K citations

    31

    h-index

  5. Continental Shelf Research

    40 publications · 2.9K citations

    29

    h-index

1–5