Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/72507
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Type: Journal article
Title: Observed relationships between extreme sub-daily precipitation, surface temperature, and relative humidity
Author: Jones, R.
Westra, S.
Sharma, A.
Citation: Geophysical Research Letters, 2010; 37(L22805):1-5
Publisher: Amer Geophysical Union
Issue Date: 2010
ISSN: 0094-8276
1944-8007
Statement of
Responsibility: 
Rhys Hardwick Jones, Seth Westra and Ashish Sharma
Abstract: Expected changes to future extreme precipitation remain a key uncertainty associated with anthropogenic climate change. Recently, extreme precipitation has been proposed to scale with the precipitable water content in the atmosphere, which assuming relative humidity stays constant, will increase at a rate of ∼6.8%/°C as indicated by the Clausius-Clapeyron (C-C) relationship. We examine this scaling empirically using data from 137 long-record pluviograph and temperature gauges across Australia. We find that scaling rates are consistent with the C-C relationship for surface temperatures up to between 20°C and 26°C and for precipitation durations up to 30 minutes, implying that such scaling applies only for individual storm systems. At greater temperatures negative scaling is observed. Consideration of relative humidity data shows a pronounced decrease in the maximum relative humidity for land surface temperatures greater than 26°C, indicating that moisture availability becomes the dominant driver of how extreme precipitation scales at higher temperatures.
Keywords: Temperature scaling; extreme precipitation; clausius-clapeyron; hydroclimatology; extreme rainfall; relative humidity
Rights: © Copyright 2010 by the American Geophysical Union.
RMID: 0020114556
DOI: 10.1029/2010GL045081
Appears in Collections:Civil and Environmental Engineering publications
Environment Institute publications

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