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    <titleInfo>
      <title>Towards improved criteria for hydrological model calibration : theoretical analysis of distance- and weak form-based functions</title>
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    <abstract>Calibrating conceptual hydrological models is often done via the optimization of objective functions serving as a measure of model performance. Most of the objective functions used in the hydrological literature can be classified into distance- and weak form-based objective functions. Distance- and weak form-based objective functions can be seen respectively as generalizations of the square error and balance error. An analysis of the objective functions shows that: (i) the calibration problem is transformed from an optimization problem with distance-based objective functions into a root finding problem for weak form-based functions; (ii) weak form-based objective functions are essentially less prone to local extrema than distance-based functions; (iii) consequently, they allow simple gradient-based methods to be used; (iv) parameter redundancy can be assessed very simply by superimposing the contour lines or comparing the gradients of two objective functions of similar nature in the parameter space; and (v) simple guidelines can be defined for the selection of the calibration variables in a conceptual hydrological model. The theoretical results are illustrated by two simple test cases. Weak form-based approaches offer the potential for better-posed calibration problems, through the use of a number of independent criteria that matches the dimension of the identification problem. In contrast with distance-based objective functions, they do not have the inconvenience of solution non-uniqueness. Finally, the need for models with internal variables bearing a physical meaning is acknowledged.</abstract>
    <targetAudience authority="marctarget">specialized</targetAudience>
    <subject>
      <topic>Model performance evaluation</topic>
      <topic>Calibration</topic>
      <topic>Objective function</topic>
      <topic>Mean squared error</topic>
      <topic>Nash-Sutcliffe efficiency</topic>
      <topic>Conceptual hydrological model</topic>
    </subject>
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      <titleInfo>
        <title>Journal of Hydrology</title>
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      <part>
        <detail type="volume">
          <number>401</number>
        </detail>
        <detail type="volume">
          <number>1-2</number>
        </detail>
        <extent unit="pages">
          <list> 1-13</list>
        </extent>
      </part>
      <originInfo>
        <dateIssued>2011</dateIssued>
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      <identifier type="issn">0022-1694</identifier>
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    <identifier type="uri">https://www.documentation.ird.fr/hor/fdi:010053501</identifier>
    <identifier type="doi">10.1016/j.jhydro.2011.02.004</identifier>
    <identifier type="issn">0022-1694</identifier>
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      <recordCreationDate encoding="w3cdtf">2011-05-31</recordCreationDate>
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