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      Improvement of hydrological model calibration by selecting multiple parameter ranges

      , , , ,
      Hydrology and Earth System Sciences
      Copernicus GmbH

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          Abstract

          <p><strong>Abstract.</strong> The parameters of hydrological models are usually calibrated to achieve good performance, owing to the highly non-linear problem of hydrology process modelling. However, parameter calibration efficiency has a direct relation with parameter range. Furthermore, parameter range selection is affected by probability distribution of parameter values, parameter sensitivity, and correlation. A newly proposed method is employed to determine the optimal combination of multi-parameter ranges for improving the calibration of hydrological models. At first, the probability distribution was specified for each parameter of the model based on genetic algorithm (GA) calibration. Then, several ranges were selected for each parameter according to the corresponding probability distribution, and subsequently the optimal range was determined by comparing the model results calibrated with the different selected ranges. Next, parameter correlation and sensibility were evaluated by quantifying two indexes, <i>R</i><sub>C <i>Y</i>, <i>X</i></sub> and <i>S</i><sub>E</sub>, which can be used to coordinate with the negatively correlated parameters to specify the optimal combination of ranges of all parameters for calibrating models. It is shown from the investigation that the probability distribution of calibrated values of any particular parameter in a Xinanjiang model approaches a normal or exponential distribution. The multi-parameter optimal range selection method is superior to the single-parameter one for calibrating hydrological models with multiple parameters. The combination of optimal ranges of all parameters is not the optimum inasmuch as some parameters have negative effects on other parameters. The application of the proposed methodology gives rise to an increase of 0.01 in minimum Nash–Sutcliffe efficiency (<i>E</i><sub>NS</sub>) compared with that of the pure GA method. The rising of minimum <i>E</i><sub>NS</sub> with little change of the maximum may shrink the range of the possible solutions, which can effectively reduce uncertainty of the model performance.</p>

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          Optimal use of the SCE-UA global optimization method for calibrating watershed models

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            Toward improved calibration of hydrologic models: Combining the strengths of manual and automatic methods

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                Author and article information

                Journal
                Hydrology and Earth System Sciences
                Hydrol. Earth Syst. Sci.
                Copernicus GmbH
                1607-7938
                2017
                January 24 2017
                : 21
                : 1
                : 393-407
                Article
                10.5194/hess-21-393-2017
                b3582a79-d695-4b54-8d22-3d61e0968765
                © 2017

                https://creativecommons.org/licenses/by/3.0/

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