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 2 Time series for a-g daily precipitation amounts greater than the 95th percentile of all wet days mm, r95p and h-n maximum consecutive five-day precipitation total mm d -1 , r5d of seven river basins of China and the trends. Red solid line: precipitation from HYD run; green dashed line: precipitation from CTL run; blue dashed line: observed precipitation. The correlation coefficients for the CTL run and HYD run compared with the observed values are also shown.