Barotropic Circulation

Barotropic Circulation is a type of ocean circulation characterized by horizontal flow that is depth-independent, in which pressure gradients arise solely from variations in sea surface height and the resultant currents are uniform throughout the water column.

298

Publications

18.1K

Citations

725

Authors

282

Institutions

Publications per year

2017–2026

26

Authors

725

  1. PD
    Peter D. Killworth

    National Oceanography Centre, United Kingdom

    6 publications · 633 citations

    6

    h-index

  2. GT
    G. T. Csanady

    Woods Hole Oceanographic Institution, United States

    4 publications · 282 citations

    4

    h-index

  3. JP
    Joseph Pedlosky

    Woods Hole Oceanographic Institution, United States

    4 publications · 86 citations

    4

    h-index

  4. CE
    Carsten Eden

    Universität Hamburg, Germany

    4 publications · 775 citations

    4

    h-index

  5. CW
    Christopher W. Hughes

    National Oceanography Centre, United Kingdom

    4 publications · 210 citations

    4

    h-index

1–5 of 725

Venues

  1. Journal of Physical Oceanography

    95 publications · 6.1K citations

    45

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 47 publications · 3.5K citations

    31

    h-index

  3. Journal of Geophysical Research Oceans

    20 publications · 1K citations

    16

    h-index

  4. Journal of the Atmospheric Sciences

    11 publications · 554 citations

    11

    h-index

  5. Geophysical Research Letters

    13 publications · 420 citations

    11

    h-index

1–5