Lifting Condensation Level
The Lifting Condensation Level is the altitude at which an air parcel, when adiabatically lifted, becomes saturated and condensation begins, marking the base of cloud formation in thermodynamic diagrams.
123
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10.6K
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370
Authors
193
Institutions
Publications per year
2017–2026
34
Variants
Lcl
123
The Computation of Equivalent Potential Temperature
David Bolton · Monthly Weather Review · 1980 · 1.7K citations
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193
NOAA National Severe Storms Laboratory
Norman, United States
13 h-index
27 publications
3.3K citations
University of Oklahoma
Norman, United States
10 h-index
17 publications
2.6K citations

NSF National Center for Atmospheric Research
Boulder, United States
10 h-index
11 publications
606 citations

Cooperative Institute for Mesoscale Meteorological Studies
Norman, United States
10 h-index
14 publications
2.3K citations
University of Maryland, College Park
College Park, United States
5 h-index
11 publications
486 citations
NOAA Storm Prediction Center
Norman, United States
5 h-index
15 publications
915 citations

Pennsylvania State University
State College, United States
5 h-index
8 publications
401 citations
University of Colorado Boulder
Boulder, United States
4 h-index
5 publications
321 citations
1–8 of 193
13 publications · 2.7K citations
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12 publications · 574 citations
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11 publications · 621 citations
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10 publications · 881 citations
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JGR · 7 publications · 402 citations
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