Conditional Instability
Conditional Instability is a thermodynamic state of the atmosphere in which an air parcel becomes buoyantly unstable and capable of sustained convection only if initially lifted to a level where condensation occurs and latent heat release provides sufficient warming to overcome the stable stratification of the environment.
143
Publications
12.4K
Citations
272
Authors
115
Institutions
Publications per year
2017–2026
12
Variants
Conditional Atmospheric Instability
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115
University of Reading
Reading, United Kingdom
12 h-index
28 publications
1.5K citations
Met Office
Exeter, United Kingdom
9 h-index
12 publications
883 citations

McGill University
Montreal, Canada
7 h-index
10 publications
334 citations

NSF National Center for Atmospheric Research
Boulder, United States
6 h-index
10 publications
412 citations
NOAA National Severe Storms Laboratory
Norman, United States
6 h-index
8 publications
635 citations
Massachusetts Institute of Technology
Cambridge, United States
6 h-index
8 publications
3.6K citations

Pennsylvania State University
State College, United States
5 h-index
9 publications
427 citations
University of Washington
Seattle, United States
5 h-index
8 publications
745 citations
1–8 of 115
37 publications · 5.6K citations
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33 publications · 2.6K citations
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20 publications · 1.6K citations
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13 publications · 662 citations
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4 publications · 428 citations
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