Vertical Pressure Gradient

Vertical Pressure Gradient is a physical gradient representing the rate of change of atmospheric or fluid pressure with respect to vertical distance, distinguished by its role in driving buoyancy and balancing gravitational forces in hydrostatic equilibrium.

204

Publications

11.5K

Citations

497

Authors

216

Institutions

Publications per year

2017–2026

26

Variants

Vertical Pressure Gradient Force

Authors

497

  1. SJ
    S. J. Lai-Fook

    University of Kentucky, United States

    5 publications · 173 citations

    5

    h-index

  2. RE
    Robert E. Hyatt

    Mayo Clinic, United States

    4 publications · 132 citations

    4

    h-index

  3. YT
    Y. Tony Song

    Jet Propulsion Laboratory, United States

    3 publications · 155 citations

    3

    h-index

  4. IJ
    I. J. Ross

    University of Kentucky, United States

    3 publications · 56 citations

    3

    h-index

  5. EA
    Emilio Agostoni

    Istituto di Fisiologia Clinica, Italy

    3 publications · 137 citations

    3

    h-index

1–5 of 497

Venues

  1. Journal of Applied Physiology

    16 publications · 774 citations

    14

    h-index

  2. Journal of the Atmospheric Sciences

    13 publications · 1.1K citations

    13

    h-index

  3. Monthly Weather Review

    12 publications · 1.3K citations

    11

    h-index

  4. Journal of Geophysical Research Atmospheres

    JGR · 10 publications · 945 citations

    10

    h-index

  5. Journal of Physical Oceanography

    8 publications · 941 citations

    8

    h-index

1–5