Barotropic Dynamics

Barotropic Dynamics is a theoretical framework in geophysical fluid dynamics that describes the large-scale motion of fluids in which density depends only on pressure, leading to depth-independent horizontal flow driven by gradients in the free surface and modulated by the Coriolis effect.

1.1K

Publications

57.7K

Citations

1.8K

Authors

680

Institutions

Publications per year

2017–2026

110

Authors

1.8K

  1. AZ
    Alexander Zlotnik

    Ben-Gurion University of the Negev, Israel

    11 publications · 219 citations

    11

    h-index

  2. GR
    Glenn R. Flierl

    Massachusetts Institute of Technology, United States

    9 publications · 867 citations

    9

    h-index

  3. IM
    Isaac M. Held

    NOAA Geophysical Fluid Dynamics Laboratory, United States

    9 publications · 777 citations

    9

    h-index

  4. RM
    Rui M. Ponte

    Atmospheric and Environmental Research, United States

    9 publications · 391 citations

    9

    h-index

  5. JC
    James C. McWilliams

    University of California, Los Angeles, United States

    8 publications · 740 citations

    8

    h-index

1–5 of 1.8K

Venues

  1. Journal of the Atmospheric Sciences

    168 publications · 11.3K citations

    56

    h-index

  2. Journal of Physical Oceanography

    150 publications · 9.2K citations

    52

    h-index

  3. Journal of Geophysical Research Atmospheres

    JGR · 80 publications · 5.2K citations

    43

    h-index

  4. Journal of Fluid Mechanics

    39 publications · 2.6K citations

    27

    h-index

  5. Monthly Weather Review

    41 publications · 1.8K citations

    24

    h-index

1–5