Advances in Meteorology / 2020 / Article / Tab 2

Research Article

Spatial Distribution and Temporal Trends in the Daily Precipitation Concentration across the Yarlung Tsangpo River Basin: Eastern Himalaya of China

Table 2

Values for the constants, a and b, of the exponential curves, coefficients of determination (R2), CI, LAC, and percentage of precipitation contributed by 25% of the rainiest days (P 25%).

StationabR2CILACP 25%

Pulan0.0230.0360.960.6460.94678
Dangxiong0.0430.0310.990.5810.89369
Lazi0.0370.0330.990.5940.89471
Rikeze0.0360.0331.000.5900.86169
Nimu0.0400.0320.990.5860.88470
Lasa0.0390.0321.000.5860.86469
Zedang0.0340.0340.990.5990.87672
Dingri0.0300.0350.990.6080.88072
Jiangzi0.0330.0340.990.6020.89172
Cuona0.0460.0300.960.5840.94672
Longzi0.0460.0300.990.5820.91371
Pali0.0460.0300.980.5850.92571
Jiali0.0400.0320.990.5860.88470
Bomi0.0290.0350.990.6120.90773
Linzhi0.0290.0350.990.6110.90073
Chayu0.0270.0350.980.6200.92174

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