Fjord Circulation

Fjord Circulation is a hydrodynamic process characterized by the net movement and vertical exchange of water masses in a fjord estuary, driven by freshwater discharge and density gradients, which establishes a two-layer flow regime distinct from other estuarine circulation types due to its strong stratification and limited tidal mixing in high-latitude coastal environments.

289

Publications

18.2K

Citations

824

Authors

287

Institutions

Publications per year

2017–2026

81

Authors

824

  1. FS
    Fiammetta Straneo

    Woods Hole Oceanographic Institution, United States

    16 publications · 1.8K citations

    16

    h-index

  2. DA
    David A. Sutherland

    University of Oregon, United States

    14 publications · 1.6K citations

    14

    h-index

  3. SR
    Søren Rysgaard

    Aarhus University, Denmark

    14 publications · 1.4K citations

    13

    h-index

  4. JM
    John Mortensen

    Grønlands Naturinstitut, Greenland

    12 publications · 1.3K citations

    11

    h-index

  5. HS
    Harald Svendsen

    University of Bergen, Norway

    11 publications · 2.2K citations

    11

    h-index

1–5 of 824

Venues

  1. Journal of Geophysical Research Oceans

    19 publications · 1.3K citations

    19

    h-index

  2. Journal of Physical Oceanography

    18 publications · 1K citations

    16

    h-index

  3. Estuarine Coastal and Shelf Science

    18 publications · 815 citations

    15

    h-index

  4. Geophysical Research Letters

    12 publications · 820 citations

    12

    h-index

  5. Continental Shelf Research

    14 publications · 812 citations

    12

    h-index

1–5