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
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11K
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468
Authors
227
Institutions
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2017–2026
35
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185
Sea breeze: Structure, forecasting, and impacts
Samuel T. K. Miller, Barry D. Keim, R. W. Talbot et al. · Reviews of Geophysics · 2003 · 589 citations · Full text
Neoclassical tearing modes and their control
Physics of Plasmas · 2006 · 379 citations
Toroidal drift modes driven by ion pressure gradients
W. Horton, Duk‐In Choi, W. M. Tang · The Physics of Fluids · 1981 · 270 citations
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Centro de Investigación Científica y de Educación Superior de Ensenada, Mexico
2 publications · 30 citations
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1–5 of 468
227
Michigan State University
East Lansing, United States
5 h-index
6 publications
371 citations
Woods Hole Oceanographic Institution
Falmouth, United States
5 h-index
8 publications
434 citations
University of Wyoming
Laramie, United States
5 h-index
9 publications
429 citations

NSF National Center for Atmospheric Research
Boulder, United States
5 h-index
12 publications
672 citations

Scripps Institution of Oceanography
La Jolla, United States
4 h-index
6 publications
126 citations
University of Wisconsin–Madison
Madison, United States
4 h-index
21 publications
683 citations
Colorado State University
Fort Collins, United States
3 h-index
7 publications
336 citations
NSF NCAR High Altitude Observatory
Boulder, United States
3 h-index
9 publications
511 citations
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JGR · 18 publications · 1.1K citations
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14 publications · 654 citations
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14 publications · 752 citations
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13 publications · 631 citations
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10 publications · 996 citations
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