Vertical Structure of Wind is a meteorological construct that characterizes the variation of wind speed and direction with height within the atmospheric boundary layer, distinguished by its focus on the vertical profile of wind dynamics as influenced by surface friction, thermal stratification, and turbulence.
343
Publications
19.3K
Citations
928
Authors
346
Institutions
Publications per year
2017–2026
55
Parents
Publications
343
1–5 of 343
Authors
928
- MC
9
h-index
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6
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- HA
6
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4
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4
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1–5 of 928
Institutions
346
NSF National Center for Atmospheric Research
Boulder, United States
14 h-index
33 publications
3.3K citations
National Oceanic and Atmospheric Administration
Washington, United States
12 h-index
35 publications
2.3K citations
University of Alaska Fairbanks
Fairbanks, United States
12 h-index
20 publications
791 citations
Kyoto University
Kyoto, Japan
11 h-index
17 publications
511 citations
Colorado State University
Fort Collins, United States
10 h-index
22 publications
2.7K citations
Chinese Academy of Sciences
Beijing, China
9 h-index
32 publications
1K citations
University of Colorado Boulder
Boulder, United States
7 h-index
12 publications
491 citations
Nanjing University of Information Science and Technology
Nanjing, China
7 h-index
12 publications
435 citations
1–8 of 346
Venues
- Journal of Geophysical Research Atmospheres
JGR · 36 publications · 2.1K citations
21
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- Quarterly Journal of the Royal Meteorological Society
23 publications · 3K citations
20
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- Journal of the Atmospheric Sciences
22 publications · 2K citations
20
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- Boundary-Layer Meteorology
21 publications · 2.1K citations
16
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- Geophysical Research Letters
18 publications · 731 citations
15
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