Geostrophic Circulation

Geostrophic Circulation is a theoretical construct in large-scale ocean circulation that describes a steady, horizontal flow of seawater in which the Coriolis force balances the horizontal pressure gradient force, arising from density variations and enabling the inference of ocean currents from hydrographic data.

913

Publications

65.5K

Citations

2K

Authors

548

Institutions

Publications per year

2017–2026

99

Authors

2K

  1. DR
    Dean Roemmich

    Scripps Institution of Oceanography, United States

    13 publications · 988 citations

    13

    h-index

  2. JL
    Joseph L. Reid

    Scripps Institution of Oceanography, United States

    9 publications · 2.7K citations

    9

    h-index

  3. MB
    Molly Baringer

    NOAA Atlantic Oceanographic and Meteorological Laboratories, United States

    8 publications · 625 citations

    8

    h-index

  4. MA
    Michael A. Spall

    Woods Hole Oceanographic Institution, United States

    8 publications · 525 citations

    8

    h-index

  5. AL
    Arnold L. Gordon

    Lamont-Doherty Earth Observatory, United States

    8 publications · 906 citations

    8

    h-index

1–5 of 2K

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 126 publications · 11.3K citations

    57

    h-index

  2. Journal of Physical Oceanography

    152 publications · 10.3K citations

    54

    h-index

  3. 26

    h-index

  4. Continental Shelf Research

    35 publications · 1.5K citations

    24

    h-index

  5. Journal of Marine Research

    30 publications · 2.1K citations

    24

    h-index

1–5