Comparison of Three Statistical Downscaling Methods and Ensemble Downscaling Method Based on Bayesian Model Averaging in Upper Hanjiang River Basin, China

Table 5

The BMA method precipitation runoff result of input analog.

Input precipitation	NSC	RC	ERR/%
Observed	0.76	0.89	−12.31
SVM	0.52	0.77	20.1
BCC/RCG-WG	0.19	0.55	5.52
SDSM	0.50	0.76	23.46
SA	0.38	0.68	18.5
BMA	0.56	0.79	13.74