Pressure-gradient Force Balance

Pressure-Gradient Force Balance is a theoretical construct in atmospheric dynamics that represents the equilibrium condition in which the pressure-gradient force is exactly balanced by the Coriolis force, resulting in steady, straight-line geostrophic flow.

74

Publications

3.3K

Citations

205

Authors

109

Institutions

Publications per year

2017–2026

15

Authors

205

  1. MK
    M. K. Yau

    McGill University, Canada

    2 publications · 193 citations

    2

    h-index

  2. AR
    A. Runov

    University of California, Los Angeles, United States

    2 publications · 109 citations

    2

    h-index

  3. KS
    K. Sakaguchi

    Nagoya University, Japan

    2 publications · 45 citations

    2

    h-index

  4. DZ
    Da‐Lin Zhang

    University of Maryland, College Park, United States

    2 publications · 193 citations

    2

    h-index

  5. ED
    E. Donovan

    University of Calgary, Canada

    2 publications · 45 citations

    2

    h-index

1–5 of 205

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 14 publications · 910 citations

    13

    h-index

  2. Monthly Weather Review

    12 publications · 662 citations

    12

    h-index

  3. Journal of the Atmospheric Sciences

    5 publications · 198 citations

    5

    h-index

  4. 5

    h-index

  5. Geophysical Research Letters

    4 publications · 183 citations

    4

    h-index

1–5