Logarithmic Wind Law
The "Logarithmic Wind Law" is a theoretical model in fluid dynamics that describes the vertical profile of wind speed in the surface layer of the atmosphere as a logarithmic function of height above the surface, accounting for surface roughness and shear stress.
58
Publications
5.5K
Citations
122
Authors
60
Institutions
Publications per year
2017–2026
10
Variants
Logarithmic Wind Profile
Parents
58
Wind stress on a water surface
H. Charnock · Quarterly Journal of the Royal Meteorological Society · 1955 · 1.9K citations
H. Tennekes · Journal of the Atmospheric Sciences · 1973 · 377 citations
1–5 of 58
122
National Institute of Standards and Technology, United States
3 publications · 83 citations
3
h-index
3
h-index
2
h-index
Commonwealth Scientific and Industrial Research Organisation, Australia
2 publications · 103 citations
2
h-index
2
h-index
1–5 of 122
60
Instituto de Ciencias Agrarias
Madrid, Spain
3 h-index
3 publications
95 citations

Newcastle University
Newcastle upon Tyne, United Kingdom
2 h-index
4 publications
120 citations
Hydroacoustics (United States)
Henrietta, United States
2 h-index
2 publications
203 citations
University of Trás-os-Montes and Alto Douro
Vila Real, Portugal
1 h-index
1 publications
15 citations
National Institute of Meteorology
Tunis, Tunisia
1 h-index
2 publications
44 citations

Pennsylvania State University
State College, United States
1 h-index
1 publications
377 citations
Center for Excellence in Tibetan Plateau Earth Sciences
Beijing, China
1 h-index
3 publications
87 citations

University of Notre Dame
Notre Dame, United States
1 h-index
3 publications
108 citations
1–8 of 60
9 publications · 2.9K citations
8
h-index
JGR · 5 publications · 515 citations
5
h-index
3 publications · 95 citations
3
h-index
3 publications · 85 citations
3
h-index
2 publications · 171 citations
2
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1–5