Cloud-topped Boundary Layers
Cloud-Topped Boundary Layer is a meteorological boundary layer regime characterized by the presence of a cloud field at its upper boundary, distinguishing it from cloud-free or decoupled boundary layer structures through the coupling of radiative, turbulent, and microphysical processes that sustain cloud persistence and influence boundary layer depth.
131
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10.8K
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354
Authors
136
Institutions
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2017–2026
15
Variants
Cloud-topped Boundary Layer
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Christopher S. Bretherton, James R. McCaa, Hervé Grenier · Monthly Weather Review · 2004 · 481 citations · Full text
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NSF National Center for Atmospheric Research, United States
12 publications · 1.8K citations
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NSF National Center for Atmospheric Research
Boulder, United States
18 h-index
27 publications
3.7K citations
University of Washington
Seattle, United States
17 h-index
45 publications
7.5K citations
Colorado State University
Fort Collins, United States
13 h-index
20 publications
3.9K citations
Met Office
Exeter, United Kingdom
12 h-index
20 publications
4.3K citations
University of California, Los Angeles
Los Angeles, United States
11 h-index
26 publications
4.6K citations
Royal Netherlands Meteorological Institute
De Bilt, The Netherlands
11 h-index
18 publications
1.1K citations

Delft University of Technology
Delft, The Netherlands
10 h-index
23 publications
736 citations
Max Planck Institute for Meteorology
Hamburg, Germany
10 h-index
18 publications
2.9K citations
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58 publications · 4.3K citations
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13 publications · 1.3K citations
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13 publications · 534 citations
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9 publications · 2.8K citations
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7 publications · 211 citations
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