Diabatic Forcing is a meteorological process within the Quasi-Geostrophic Theory that represents the rate of change of potential temperature due to non-adiabatic heat sources or sinks, such as radiation, latent heat release, and surface fluxes, distinguishing it from adiabatic processes governed solely by pressure-volume work.
211
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Citations
522
Authors
179
Institutions
Publications per year
2017–2026
50
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211
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Institutions
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University of Reading
Reading, United Kingdom
16 h-index
50 publications
4.2K citations
ETH Zurich
Zurich, Switzerland
14 h-index
38 publications
3.1K citations
NSF National Center for Atmospheric Research
Boulder, United States
10 h-index
15 publications
3K citations
Colorado State University
Fort Collins, United States
9 h-index
15 publications
1.2K citations
Centre National de la Recherche Scientifique
Paris, France
9 h-index
33 publications
1.6K citations
National Centre for Atmospheric Science
Leeds, United Kingdom
9 h-index
26 publications
1.9K citations
Met Office
Exeter, United Kingdom
8 h-index
22 publications
1.6K citations
Karlsruhe Institute of Technology
Karlsruhe, Germany
7 h-index
16 publications
2.1K citations
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Venues
- Journal of the Atmospheric Sciences
54 publications · 3.1K citations
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- Monthly Weather Review
40 publications · 1.8K citations
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- Quarterly Journal of the Royal Meteorological Society
26 publications · 2.2K citations
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- Journal of Climate
18 publications · 945 citations
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- Journal of Physical Oceanography
13 publications · 856 citations
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