Geostrophic Flow

Geostrophic Flow is a steady oceanic flow in which the pressure gradient force is balanced by the Coriolis force, resulting in motion parallel to the isobars.

2.9K

Publications

170.6K

Citations

5.3K

Authors

1.3K

Institutions

Publications per year

2017–2026

280

Authors

5.3K

  1. JC
    James C. McWilliams

    University of California, Los Angeles, United States

    24 publications · 2.4K citations

    22

    h-index

  2. BJ
    Brian J. Hoskins

    University of Reading, United Kingdom

    15 publications · 3.6K citations

    15

    h-index

  3. DG
    David G. Dritschel

    University of St Andrews, United Kingdom

    23 publications · 794 citations

    15

    h-index

  4. VZ
    Vladimir Zeitlin

    Laboratoire de Météorologie Dynamique, France

    15 publications · 755 citations

    14

    h-index

  5. GR
    Glenn R. Flierl

    Massachusetts Institute of Technology, United States

    14 publications · 1K citations

    13

    h-index

1–5 of 5.3K

Venues

  1. Journal of Physical Oceanography

    335 publications · 20.2K citations

    75

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 245 publications · 16.9K citations

    71

    h-index

  3. Journal of the Atmospheric Sciences

    196 publications · 15.4K citations

    63

    h-index

  4. Journal of Fluid Mechanics

    173 publications · 8.7K citations

    57

    h-index

  5. Monthly Weather Review

    84 publications · 3.6K citations

    37

    h-index

1–5