Boundary Layer Decoupling
Boundary Layer Decoupling is a meteorological phenomenon in which the convective boundary layer becomes stratified into distinct sublayers, characterized by the suppression of turbulent exchange between the surface-driven mixed layer and the overlying air, thereby inhibiting vertical communication of heat, moisture, and momentum in the lower atmosphere.
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5.3K
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281
Authors
120
Institutions
Publications per year
2017–2026
18
81
100 Years of Research on Mesoscale Convective Systems
Robert A. Houze · Meteorological Monographs · 2018 · 269 citations · Full text
A Climatology of Nocturnal Low-Level Jets at Cabauw
Peter Baas, Fred C. Bosveld, H. Klein Baltink et al. · Journal of Applied Meteorology and Climatology · 2009 · 209 citations · Full text
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London School of Hygiene & Tropical Medicine, United Kingdom
3 publications · 422 citations
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3
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1–5 of 281
120
Met Office
Exeter, United Kingdom
10 h-index
19 publications
1.1K citations

NSF National Center for Atmospheric Research
Boulder, United States
10 h-index
32 publications
1.1K citations
University of Washington
Seattle, United States
9 h-index
26 publications
3.5K citations
Météo-France
Toulouse, France
5 h-index
11 publications
1K citations
University of Miami
Coral Gables, United States
5 h-index
15 publications
749 citations

Centre National de la Recherche Scientifique
Paris, France
5 h-index
13 publications
1.2K citations
University of Reading
Reading, United Kingdom
4 h-index
6 publications
106 citations

United States Naval Research Laboratory
Washington, United States
3 h-index
7 publications
340 citations
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16 publications · 1.5K citations
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10 publications · 538 citations
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7 publications · 548 citations
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5 publications · 225 citations
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4 publications · 183 citations
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