Gradient Wind Balance

Gradient Wind Balance is a steady-state wind balance condition in curved atmospheric flows wherein the pressure gradient force, Coriolis force, and centrifugal force are in mutual equilibrium, extending geostrophic balance to account for flow curvature.

66

Publications

4.1K

Citations

150

Authors

93

Institutions

Publications per year

2017–2026

12

Authors

150

  1. MT
    Michael T. Montgomery

    Naval Postgraduate School, United States

    11 publications · 802 citations

    10

    h-index

  2. JC
    James C. McWilliams

    University of California, Los Angeles, United States

    7 publications · 379 citations

    7

    h-index

  3. RK
    Roger K. Smith

    Ludwig-Maximilians-Universität München, Germany

    7 publications · 577 citations

    7

    h-index

  4. DS
    David S. Nolan

    University of Miami, United States

    5 publications · 215 citations

    5

    h-index

  5. JD
    Jeffrey D. Kepert

    Bureau of Meteorology, Australia

    4 publications · 384 citations

    4

    h-index

1–5 of 150

Venues

  1. Journal of the Atmospheric Sciences

    18 publications · 1.9K citations

    16

    h-index

  2. Monthly Weather Review

    13 publications · 516 citations

    12

    h-index

  3. Journal of Physical Oceanography

    8 publications · 271 citations

    8

    h-index

  4. 7

    h-index

  5. Journal of Fluid Mechanics

    3 publications · 186 citations

    3

    h-index

1–5