Downscaling GCMs Using the Smooth Support Vector Machine Method to Predict Daily Precipitation in the Hanjiang Basin

作     者：陈华 郭靖 熊伟 郭生练 Chong-Yu XU CHEN Hua;GUO Jin;XIONG Wei;GUO Shenglia;Chong-Yu XU

作者机构：State Key Laboratory o/Water Resources and Hydropower Engineering ScienceWuhan University Wuhan 430072 Department of Geosciences University of Oslo PO Box 1047 Blindern NO-0316 Oslo Nomvay Radar and Avionics Institute of Aviation Industry Corporation of China Wuxi 214063 

出 版 物：《Advances in Atmospheric Sciences》 (大气科学进展（英文版）)

年 卷 期：2010年第27卷第2期

页      面：274-284页

核心收录：

学科分类：07[理学] 070601[理学-气象学] 0706[理学-大气科学] 

基　　金：supported financially by the National Natural Science Foundation of China (Grant Nos.50679063 and 50809049) the International CooperationResearch Fund of China (2005DFA20520) the Re-search Fund for the Doctoral Program of Higher Education(200804861062) 

主　　题：SSVM GCM statistical downscaling precipitation Hanjiang Basin 

摘      要：General circulation models （GCMs） are often used in assessing the impact of climate change at global and continental scales. However, the climatic factors simulated by GCMs are inconsistent at comparatively smaller scales, such as individual river basins. In this study, a statistical downscaling approach based on the Smooth Support Vector Machine （SSVM） method was constructed to predict daily precipitation of the changed climate in the Hanjiang Basin. NCEP/NCAR reanalysis data were used to establish the statistical relationship between the larger scale climate predictors and observed precipitation. The relationship obtained was used to project future precipitation from two GCMs （CGCM2 and HadCM3） for the A2 emission scenario. The results obtained using SSVM were compared with those from an artificial neural network （ANN）. The comparisons showed that SSVM is suitable for conducting climate impact studies as a statistical downscaling tool in this region. The temporal trends projected by SSVM based on the A2 emission scenario for CGCM2 and HadCM3 were for rainfall to decrease during the period 2011–2040 in the upper basin and to increase after 2071 in the whole of Hanjiang Basin.