Data of the RSYZ.xlsx

Based on the analysis of the measured data in the source area of the Yangtze River, the change of runoff and sediment is determined and the response mechanism of the change of runoff and sediment flux to climate change is obtained. Precipitation and Temperature data came from the average of four meteorological stations in Tuotuo River, Wudaoliang, Qumalai and Yushu. The data of runoff and sediment flux are derived from Zhimenda hydrology station, a control station in the source area of the Yangtze River.