Gradient Wind Balance
Gradient Wind Balance is a steady-state wind balance condition in curved atmospheric flows wherein the pressure gradient force, Coriolis force, and centrifugal force are in mutual equilibrium, extending geostrophic balance to account for flow curvature.
66
Publications
4.1K
Citations
150
Authors
93
Institutions
Publications per year
2017–2026
12
66
Gradient Balance in Tropical Cyclones
H. E. Willoughby · Journal of the Atmospheric Sciences · 1990 · 166 citations · Full text
Asymmetric and axisymmetric dynamics of tropical cyclones
John Persing, Michael T. Montgomery, James C. McWilliams et al. · Atmospheric chemistry and physics · 2013 · 151 citations · Full text
1–5 of 66
150
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University of California, Los Angeles, United States
7 publications · 379 citations
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93

Naval Postgraduate School
Monterey, United States
9 h-index
13 publications
1.1K citations

Bureau of Meteorology
Melbourne, Australia
6 h-index
9 publications
483 citations
Colorado State University
Fort Collins, United States
6 h-index
8 publications
582 citations
University of Miami
Coral Gables, United States
6 h-index
9 publications
229 citations
National Oceanic and Atmospheric Administration
Washington, United States
5 h-index
5 publications
381 citations
University of California, Los Angeles
Los Angeles, United States
4 h-index
5 publications
362 citations
Ludwig-Maximilians-Universität München
Munich, Germany
4 h-index
6 publications
584 citations

NSF National Center for Atmospheric Research
Boulder, United States
3 h-index
5 publications
221 citations
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18 publications · 1.9K citations
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13 publications · 516 citations
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8 publications · 271 citations
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7 publications · 515 citations
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3 publications · 186 citations
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