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%).

Station	a	b	R^2	CI	LAC	P 25%
Pulan	0.023	0.036	0.96	0.646	0.946	78
Dangxiong	0.043	0.031	0.99	0.581	0.893	69
Lazi	0.037	0.033	0.99	0.594	0.894	71
Rikeze	0.036	0.033	1.00	0.590	0.861	69
Nimu	0.040	0.032	0.99	0.586	0.884	70
Lasa	0.039	0.032	1.00	0.586	0.864	69
Zedang	0.034	0.034	0.99	0.599	0.876	72
Dingri	0.030	0.035	0.99	0.608	0.880	72
Jiangzi	0.033	0.034	0.99	0.602	0.891	72
Cuona	0.046	0.030	0.96	0.584	0.946	72
Longzi	0.046	0.030	0.99	0.582	0.913	71
Pali	0.046	0.030	0.98	0.585	0.925	71
Jiali	0.040	0.032	0.99	0.586	0.884	70
Bomi	0.029	0.035	0.99	0.612	0.907	73
Linzhi	0.029	0.035	0.99	0.611	0.900	73
Chayu	0.027	0.035	0.98	0.620	0.921	74