Detecting Changes in Precipitation and Temperature Extremes over China Using a Regional Climate Model with Water Table Dynamics Considered
QIN Pei-Hua1, XIE Zheng-Hui1, WANG Ai-Wen1,2
Figure 3 a-d Diagnostic plots from fitting observed daily precipitation, e-h daily precipitation from the CTL run, and i-l HYD run to the GP distribution in the Haihe River Basin from 1 September 1982 to 28 August 2002 .