Super‐Clausius–Clapeyron scaling of rainfall in a model squall line
The sensitivity of squall rainfall to changes in atmospheric temperature is investigated. For instantaneous rainrates and accumulations up to one hour, extreme rainfall scales with Clausius‐Clapeyron (CC) for temperatures below 24°C and at up to twice CC above 24°C. For longer accumulation periods a...
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| Veröffentlicht in: | Quarterly journal of the Royal Meteorological Society Jg. 139; H. 671; S. 334 - 339 |
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| Sprache: | Englisch |
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Chichester, UK
John Wiley & Sons, Ltd
01.01.2013
Wiley Subscription Services, Inc |
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| Abstract | The sensitivity of squall rainfall to changes in atmospheric temperature is investigated. For instantaneous rainrates and accumulations up to one hour, extreme rainfall scales with Clausius‐Clapeyron (CC) for temperatures below 24°C and at up to twice CC above 24°C. For longer accumulation periods and higher temperatures the scaling breaks down due to increased propagation of the squall line. For all periods, the storm average rainfall is found to scale at approximately 1.5 times CC over the entire range of temperatures. These results have implications for design parameters for infrastructure that is vulnerable to flooding and for climate change projections. Copyright © 2012 Royal Meteorological Society |
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| AbstractList | The sensitivity of squall rainfall to changes in atmospheric temperature is investigated. For instantaneous rainrates and accumulations up to one hour, extreme rainfall scales with Clausius‐Clapeyron (CC) for temperatures below 24°C and at up to twice CC above 24°C. For longer accumulation periods and higher temperatures the scaling breaks down due to increased propagation of the squall line. For all periods, the storm average rainfall is found to scale at approximately 1.5 times CC over the entire range of temperatures. These results have implications for design parameters for infrastructure that is vulnerable to flooding and for climate change projections. Copyright © 2012 Royal Meteorological Society The sensitivity of squall rainfall to changes in atmospheric temperature is investigated. For instantaneous rainrates and accumulations up to one hour, extreme rainfall scales with Clausius-Clapeyron (CC) for temperatures below 24 degree C and at up to twice CC above 24 degree C. For longer accumulation periods and higher temperatures the scaling breaks down due to increased propagation of the squall line. For all periods, the storm average rainfall is found to scale at approximately 1.5 times CC over the entire range of temperatures. These results have implications for design parameters for infrastructure that is vulnerable to flooding and for climate change projections. Copyright [copy 2012 Royal Meteorological Society The sensitivity of squall rainfall to changes in atmospheric temperature is investigated. For instantaneous rainrates and accumulations up to one hour, extreme rainfall scales with Clausius-Clapeyron (CC) for temperatures below 24°C and at up to twice CC above 24°C. For longer accumulation periods and higher temperatures the scaling breaks down due to increased propagation of the squall line. For all periods, the storm average rainfall is found to scale at approximately 1.5 times CC over the entire range of temperatures. These results have implications for design parameters for infrastructure that is vulnerable to flooding and for climate change projections. Copyright © 2012 Royal Meteorological Society [PUBLICATION ABSTRACT] |
| Author | Toumi, Ralf Singleton, Andrew |
| Author_xml | – sequence: 1 givenname: Andrew surname: Singleton fullname: Singleton, Andrew – sequence: 2 givenname: Ralf surname: Toumi fullname: Toumi, Ralf email: r.toumi@imperial.ac.uk |
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| SubjectTerms | Accumulations Atmospheric temperature Clausius–Clapeyron scaling Climate change Copyrights Design parameters Extreme weather Flooding High temperature PMP probable maximum precipitation Rainfall rainfall extremes Reproduction Squalls |
| Title | Super‐Clausius–Clapeyron scaling of rainfall in a model squall line |
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