Research Article

Uncertainty Analysis of Multiple Hydrologic Models Using the Bayesian Model Averaging Method

Table 2

Results of BMA and its 9 individual models in the mean prediction and 90% uncertainty interval for the whole flow series.

Objective functionModelsMean prediction90% uncertainty interval
(%)DRMSRE (%)CR (%) (m3/s) (m3/s)

Calibration period
OF2 (MSEST)XAJ85.45 34.89 30.24 17.89 29.43 21.46
SMAR84.61 35.89 6.96 31.67 36.51 19.30
SIM80.73 40.17 31.51 15.39 28.47 22.67
OF3 (MSESRT)XAJ89.78 29.25 10.44 68.06 33.37 11.75
SMAR80.25 40.66 10.13 44.17 35.37 17.39
SIM72.42 48.05 5.82 47.72 42.57 21.26
OF4 (MSELT)XAJ79.99 40.93 12.39 63.94 33.92 14.75
SMAR58.01 59.29 −9.22 42.28 43.45 28.32
SIM52.71 62.92 −41.07 38.89 55.51 26.93

BMA 90.49 28.22 21.40 91.11 70.98 14.54

Validation period
OF2 (MSEST)XAJ82.70 32.21 31.92 14.79 21.56 18.20
SMAR80.05 34.59 0.66 30.23 29.52 16.64
SIM69.81 42.56 39.48 20.84 24.43 22.32
OF3 (MSESRT)XAJ88.52 26.25 4.54 68.56 26.95 9.62
SMAR78.26 36.11 7.48 44.56 27.59 14.53
SIM71.09 41.64 8.98 53.86 27.69 16.47
OF4 (MSELT)XAJ77.25 36.94 8.74 63.07 26.68 11.85
SMAR43.43 58.25 −18.79 35.53 35.76 27.36
SIM72.27 40.79 −21.69 34.05 36.22 18.96

BMA 84.54 30.46 25.42 90.23 55.91 13.20

Note: bolded values represent the best results.