Advances in Meteorology / 2016 / Article / Tab 3

Research Article

Improving the Distributed Hydrological Model Performance in Upper Huai River Basin: Using Streamflow Observations to Update the Basin States via the Ensemble Kalman Filter

Table 3

Error parameters in the synthetic experiment.

VariablesError distributionMeanStandard deviationBound

PrecipitationGaussian, multiplicative10.2(0, —)
Predicted states Gaussian, multiplicative10.01(0, —)
Predicted streamflowGaussian, multiplicative10.2(0, —)
Parameters Gaussian distribution1Given in Table 4
Observed streamflowGaussian, multiplicative10.1(0, —)

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