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Sources and sinks of entropy in the atmosphere
Moist entropy is generally treated as a conserved variable in atmospheric models in the absence of external heat and moisture sources such as radiation and surface fluxes. However, both irreversible generation and nonadvective transport of entropy occur in the atmosphere, with many of these associat...
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Published in: | Journal of advances in modeling earth systems 2013-12, Vol.5 (4), p.755-763 |
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Main Author: | |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Request full text |
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Summary: | Moist entropy is generally treated as a conserved variable in atmospheric models in the absence of external heat and moisture sources such as radiation and surface fluxes. However, both irreversible generation and nonadvective transport of entropy occur in the atmosphere, with many of these associated with moisture and precipitation. These entropy sources and sinks are needed to balance the global entropy budget. Existing work on calculating the irreversible generation of entropy and nonadvective transport is extended to include the major effects of ice.
Key Points
The moist entropy budget must be treated correctly in climate models
A means of eliminating numerical entropy sources in models is presented
Physical entropy sources in the atmosphere are assessed |
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ISSN: | 1942-2466 1942-2466 |
DOI: | 10.1002/jame.20050 |