Stable Boundary Layer Flows is a meteorological phenomenon characterized by stratified, low-turbulence airflow in the lowest portion of the atmosphere where temperature increases with height, inhibiting vertical mixing and prevailing during nighttime or under strong surface cooling in mountain-valley environments.
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335
An Intercomparison of Large-Eddy Simulations of the Stable Boundary Layer
Robert J. Beare, M. K. MacVean, A.A.M. Holtslag et al. · Boundary-Layer Meteorology · 2006 · 551 citations · Full text
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303
Wageningen University & Research
Wageningen, The Netherlands
20 h-index
62 publications
4.9K citations
Cooperative Institute for Research in Environmental Sciences
Boulder, United States
19 h-index
41 publications
4.8K citations
NSF National Center for Atmospheric Research
Boulder, United States
18 h-index
50 publications
10.8K citations
Met Office
Exeter, United Kingdom
17 h-index
35 publications
3.9K citations
University of Colorado Boulder
Boulder, United States
16 h-index
44 publications
9.7K citations
Universidade Federal de Santa Maria
Santa Maria, Brazil
14 h-index
45 publications
1.9K citations
NOAA Earth System Research Laboratory
Boulder, United States
14 h-index
38 publications
4.3K citations
Northwest Research Associates
Redmond, United States
13 h-index
29 publications
8K citations
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Venues
- Boundary-Layer Meteorology
100 publications · 6.9K citations
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- Journal of the Atmospheric Sciences
42 publications · 3.5K citations
28
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- Quarterly Journal of the Royal Meteorological Society
35 publications · 2K citations
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- Bulletin of the American Meteorological Society
BAMS · 10 publications · 1.3K citations
10
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- Journal of Geophysical Research Atmospheres
JGR · 10 publications · 454 citations
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