Statistical downscaling of extreme daily precipitation,evaporation, and temperature and construction of future scenarios |
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Authors: | Tao Yang Huihui Li Weiguang Wang Chong‐Yu Xu Zhongbo Yu |
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Affiliation: | 1. (+86) 25 8378 6017(+86) 25 8378 6606;2. State Key Laboratory of Hydrology‐ Water Resources and Hydraulics Engineering, Hohai University, , Nanjing, 210098 China;3. Department of Geosciences, University of Oslo, , Blindern, 0316 Oslo, Norway;4. Department of Geoscience, University of Nevada Las Vegas, , Las Vegas, NV89154 USA |
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Abstract: | Generally, the statistical downscaling approaches work less perfectly in reproducing precipitation than temperatures, particularly for the extreme precipitation. This article aimed to testify the capability in downscaling the extreme temperature, evaporation, and precipitation in South China using the statistical downscaling method. Meanwhile, the linkages between the underlying driving forces and the incompetent skills in downscaling precipitation extremes over South China need to be extensively addressed. Toward this end, a statistical downscaling model (SDSM) was built up to construct future scenarios of extreme daily temperature, pan evaporation, and precipitation. The model was thereafter applied to project climate extremes in the Dongjiang River basin in the 21st century from the HadCM3 (Hadley Centre Coupled Model version 3) model under A2 and B2 emission scenarios. The results showed that: (1) The SDSM generally performed fairly well in reproducing the extreme temperature. For the extreme precipitation, the performance of the model was less satisfactory than temperature and evaporation. (2) Both A2 and B2 scenarios projected increases in temperature extremes in all seasons; however, the projections of change in precipitation and evaporation extremes were not consistent with temperature extremes. (3) Skills of SDSM to reproduce the extreme precipitation were very limited. This was partly due to the high randomicity and nonlinearity dominated in extreme precipitation process over the Dongjiang River basin. In pre‐flood seasons (April to June), the mixing of the dry and cold air originated from northern China and the moist warm air releases excessive rainstorms to this basin, while in post‐flood seasons (July to October), the intensive rainstorms are triggered by the tropical system dominated in South China. These unique characteristics collectively account for the incompetent skills of SDSM in reproducing precipitation extremes in South China. Copyright © 2011 John Wiley & Sons, Ltd. |
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Keywords: | climate extremes statistical downscaling climate change projection scenarios |
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