Pressure-gradient Force Balance
Pressure-Gradient Force Balance is a theoretical construct in atmospheric dynamics that represents the equilibrium condition in which the pressure-gradient force is exactly balanced by the Coriolis force, resulting in steady, straight-line geostrophic flow.
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2017–2026
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Robert H. Weisberg, Lianyuan Zheng · Journal of Geophysical Research Atmospheres · 2008 · 123 citations · Full text
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University of California, Los Angeles
Los Angeles, United States
4 h-index
12 publications
640 citations
Planetary Science Institute
Tucson, United States
3 h-index
9 publications
451 citations
University of Maryland, College Park
College Park, United States
3 h-index
5 publications
295 citations
Eindhoven University of Technology
Eindhoven, The Netherlands
2 h-index
8 publications
315 citations
Princeton University
Princeton, United States
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7 publications
214 citations
University of Michigan
Ann Arbor, United States
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2 publications
118 citations

University of Calgary
Calgary, Canada
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4 publications
90 citations

Naval Postgraduate School
Monterey, United States
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2 publications
35 citations
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JGR · 14 publications · 910 citations
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12 publications · 662 citations
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5 publications · 80 citations
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