Ageostrophic Flow

Ageostrophic Flow is a type of atmospheric flow representing the deviation of actual wind from the geostrophic wind, arising due to imbalances between the Coriolis force and the pressure gradient force, particularly in regions of curved flow, frictional effects, or rapid acceleration within the Ekman layer.

443

Publications

22.1K

Citations

935

Authors

344

Institutions

Publications per year

2017–2026

75

Authors

935

  1. JC
    James C. McWilliams

    University of California, Los Angeles, United States

    18 publications · 1.8K citations

    18

    h-index

  2. JT
    Joaquı́n Tintoré

    Mediterranean Institute for Advanced Studies, Spain

    10 publications · 837 citations

    10

    h-index

  3. MJ
    M. Jeroen Molemaker

    University of California, Los Angeles, United States

    9 publications · 1.3K citations

    9

    h-index

  4. DK
    Daniel Keyser

    University at Albany, State University of New York, United States

    7 publications · 354 citations

    7

    h-index

  5. LN
    Leif N. Thomas

    Stanford University, United States

    7 publications · 637 citations

    7

    h-index

1–5 of 935

Venues

  1. Journal of Physical Oceanography

    77 publications · 5.7K citations

    39

    h-index

  2. Journal of the Atmospheric Sciences

    73 publications · 3.4K citations

    31

    h-index

  3. Monthly Weather Review

    58 publications · 2.2K citations

    27

    h-index

  4. 23

    h-index

  5. Journal of Geophysical Research Atmospheres

    JGR · 33 publications · 1.7K citations

    22

    h-index

1–5