Wind Speed-up Effects
Wind Speed-Up Effects is the phenomenon in atmospheric boundary layer dynamics wherein wind velocity increases over elevated terrain features due to flow convergence and conservation of mass, distinguishing it from other terrain-induced flow modifications by its specific dependence on topographic slope and upstream flow conditions.
14
Publications
772
Citations
43
Authors
18
Institutions
Publications per year
2017–2026
3
Parents
14
1–5 of 14
43
2
h-index
1
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1
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NOAA Center for Satellite Applications and Research, United States
1 publications · 12 citations
1
h-index
1–5 of 43
18

Western University
London, Canada
2 h-index
4 publications
297 citations
University of Guelph
Guelph, Canada
2 h-index
2 publications
150 citations
Zhejiang University of Water Resource and Electric Power
Hangzhou, China
1 h-index
1 publications
12 citations

University of Auckland
Auckland, New Zealand
1 h-index
2 publications
82 citations

Zhejiang University
Hangzhou, China
1 h-index
3 publications
36 citations
Technological Educational Institute of Piraeus
Aigáleo, Greece
1 h-index
1 publications
11 citations
East Carolina University
Greenville, United States
1 h-index
1 publications
26 citations

University of British Columbia
Vancouver, Canada
1 h-index
1 publications
66 citations
1–8 of 18
3 publications · 247 citations
3
h-index
2 publications · 57 citations
2
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2 publications · 92 citations
2
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1 publications · 230 citations
1
h-index
1 publications · 12 citations
1
h-index
1–5