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
Parents
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Oregon State University
Corvallis, United States
5 h-index
10 publications
205 citations

Delft University of Technology
Delft, The Netherlands
3 h-index
8 publications
1.2K citations
NOAA National Severe Storms Laboratory
Norman, United States
3 h-index
5 publications
232 citations

Scripps Institution of Oceanography
La Jolla, United States
3 h-index
3 publications
477 citations
Colorado State University
Fort Collins, United States
3 h-index
4 publications
136 citations

Chinese Academy of Sciences
Beijing, China
3 h-index
16 publications
3K citations
Jet Propulsion Laboratory
Pasadena, United States
3 h-index
3 publications
155 citations
University of Michigan
Ann Arbor, United States
2 h-index
3 publications
125 citations
1–8 of 216
16 publications · 774 citations
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13 publications · 1.1K citations
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12 publications · 1.3K citations
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JGR · 10 publications · 945 citations
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8 publications · 941 citations
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1–5