CMIP5 downscaling and its uncertainty in China

• Published in: Global and planetary change 2016-11, Vol.146, p.30-37
• Main Authors: Yue, TianXiang, Zhao, Na, Fan, ZeMeng, Li, Jing, Chen, ChuanFa, Lu, YiMin, Wang, ChenLiang, Xu, Bing, Wilson, John
• Format: Article
• Language: English
• Subjects: Annual precipitation; Climate scenarios; Downscaling; Elevation; HASM-GB; HASM-OLS; Independent variables; Latitude; Regression; Spatial stationarity, non-stationarity; Stations; Tibet; Uncertainty
• ISSN: 0921-8181; 1872-6364
• DOI: 10.1016/j.gloplacha.2016.09.003

A comparison between the Coupled Model Intercomparison Project Phase 5 (CMIP5) data and observations at 735 meteorological stations indicated that mean annual temperature (MAT) was underestimated about 1.8°C while mean annual precipitation (MAP) was overestimated about 263mm in general across the whole of China. A statistical analysis of China-CMIP5 data demonstrated that MAT exhibits spatial stationarity, while MAP exhibits spatial non-stationarity. MAT and MAP data from the China-CMIP5 dataset were downscaled by combining statistical approaches with a method for high accuracy surface modeling (HASM). A statistical transfer function (STF) of MAT was formulated using minimized residuals output by HASM with an ordinary least squares (OLS) linear equation that used latitude and elevation as independent variables, abbreviated as HASM-OLS. The STF of MAP under a BOX-COX transformation was derived as a combination of minimized residuals output by HASM with a geographically weight regression (GWR) using latitude, longitude, elevation and impact coefficient of aspect as independent variables, abbreviated as HASM-GB. Cross validation, using observational data from the 735 meteorological stations across China for the period 1976 to 2005, indicates that the largest uncertainty occurred on the Tibet plateau with mean absolute errors (MAEs) of MAT and MAP as high as 4.64°C and 770.51mm, respectively. The downscaling processes of HASM-OLS and HASM-GB generated MAEs of MAT and MAP that were 67.16% and 77.43% lower, respectively across the whole of China on average, and 88.48% and 97.09% lower for the Tibet plateau. •Mean annual temperature (MAT) was underestimated about 1.8°C by CMIP5.•mean annual precipitation (MAP) was overestimated about 263 mm.•MAT and MAP data from the China-CMIP5 dataset were downscaled by using a method for high accuracy surface modeling (HASM).•The downscaling processes decreased mean absolute errors (MAEs) of MAT and MAP by 67.16% and 77.43% respectively.