Stable Boundary Layer Effects
Stable Boundary Layer Effects is a meteorological phenomenon characterized by the suppression of turbulent mixing in the atmospheric boundary layer due to a temperature inversion, typically occurring at night or in valley bottoms, which enhances the persistence and structure of downslope and down-valley winds.
49
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5.9K
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169
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93
Institutions
Publications per year
2017–2026
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Michael Ek, Kenneth E. Mitchell, Ying Lin et al. · Journal of Geophysical Research Atmospheres · 2003 · 3.3K citations · Full text
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Cooperative Institute for Research in Environmental Sciences, United States
2 publications · 78 citations
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NSF National Center for Atmospheric Research, United States
2 publications · 99 citations
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Met Office
Exeter, United Kingdom
5 h-index
8 publications
585 citations
Wageningen University & Research
Wageningen, The Netherlands
4 h-index
10 publications
621 citations
Northwest Research Associates
Redmond, United States
3 h-index
3 publications
108 citations

British Antarctic Survey
Cambridge, United Kingdom
3 h-index
5 publications
157 citations
University of Oklahoma
Norman, United States
3 h-index
14 publications
903 citations

Nanjing University of Information Science and Technology
Nanjing, China
3 h-index
4 publications
233 citations
Cooperative Institute for Research in Environmental Sciences
Boulder, United States
3 h-index
5 publications
167 citations

NSF National Center for Atmospheric Research
Boulder, United States
2 h-index
4 publications
81 citations
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18 publications · 1.2K citations
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BAMS · 3 publications · 91 citations
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3 publications · 159 citations
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JGR · 2 publications · 3.3K citations
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2 publications · 124 citations
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