Low-stratus Boundary Layers
Low-Stratus Boundary Layers is a meteorological construct denoting a type of atmospheric boundary layer characterized by the persistent presence of a shallow, horizontally extensive stratus cloud deck that forms and sustains within a stably stratified layer near the Earth's surface, primarily driven by radiative cooling, turbulent mixing, and cloud-top entrainment processes unique to low-cloud regimes.
25
Publications
2.2K
Citations
44
Authors
25
Institutions
Publications per year
2017–2026
1
25
1–5 of 25
44
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2 publications · 80 citations
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25

Johns Hopkins University
Baltimore, United States
2 h-index
2 publications
71 citations
ETH Zurich
Zurich, Switzerland
2 h-index
3 publications
655 citations
University of Wyoming
Laramie, United States
2 h-index
5 publications
89 citations

Uppsala University
Uppsala, Sweden
2 h-index
2 publications
27 citations
Stanford University
Stanford, United States
1 h-index
2 publications
128 citations
Philipps University of Marburg
Marburg, Germany
1 h-index
1 publications
138 citations
RWTH Aachen University
Aachen, Germany
1 h-index
1 publications
27 citations

Finnish Meteorological Institute
Helsinki, Finland
1 h-index
1 publications
54 citations
1–8 of 25
5 publications · 1.1K citations
5
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4 publications · 116 citations
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3 publications · 180 citations
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2 publications · 23 citations
2
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JGR · 2 publications · 101 citations
2
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1–5