Pressure Gradient Forcing

Pressure Gradient Forcing is a meteorological phenomenon characterized as a force per unit mass arising from spatial variations in atmospheric pressure, distinctively driving the acceleration of air parcels within valley wind systems.

185

Publications

11K

Citations

468

Authors

227

Institutions

Publications per year

2017–2026

35

Authors

468

  1. TR
    Thomas R. Parish

    University of Wyoming, United States

    4 publications · 199 citations

    4

    h-index

  2. BV
    B.J.H. van de Wiel

    Delft University of Technology, Netherlands

    2 publications · 173 citations

    2

    h-index

  3. DG
    D. G. Steyn

    University of British Columbia, Canada

    2 publications · 49 citations

    2

    h-index

  4. ML
    Manuel López

    Centro de Investigación Científica y de Educación Superior de Ensenada, Mexico

    2 publications · 30 citations

    2

    h-index

  5. CD
    C. David Whiteman

    University of Utah, United States

    2 publications · 59 citations

    2

    h-index

1–5 of 468

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 18 publications · 1.1K citations

    16

    h-index

  2. Monthly Weather Review

    14 publications · 654 citations

    13

    h-index

  3. Journal of Physical Oceanography

    14 publications · 752 citations

    13

    h-index

  4. Journal of the Atmospheric Sciences

    13 publications · 631 citations

    12

    h-index

  5. Journal of Fluid Mechanics

    10 publications · 996 citations

    10

    h-index

1–5