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      <ref-type name="Journal Article">17</ref-type>
      <work-type>ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES</work-type>
      <contributors>
        <authors>
          <author>
            <style face="normal" font="default" size="100%">Guinot, V.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Cappelaere, Bernard</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Delenne, C.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Ruelland, D.</style>
          </author>
        </authors>
      </contributors>
      <titles>
        <title>Towards improved criteria for hydrological model calibration : theoretical analysis of distance- and weak form-based functions</title>
        <secondary-title>Journal of Hydrology</secondary-title>
      </titles>
      <pages>1-13</pages>
      <keywords>
        <keyword>Model performance evaluation</keyword>
        <keyword>Calibration</keyword>
        <keyword>Objective function</keyword>
        <keyword>Mean squared error</keyword>
        <keyword>Nash-Sutcliffe efficiency</keyword>
        <keyword>Conceptual hydrological model</keyword>
      </keywords>
      <dates>
        <year>2011</year>
      </dates>
      <call-num>fdi:010053501</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Journal of Hydrology</full-title>
      </periodical>
      <isbn>0022-1694</isbn>
      <accession-num>ISI:000290072000001</accession-num>
      <number>1-2</number>
      <electronic-resource-num>10.1016/j.jhydro.2011.02.004</electronic-resource-num>
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          <url>https://www.documentation.ird.fr/hor/fdi:010053501</url>
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          <url>https://www.documentation.ird.fr/intranet/publi/2011/05/010053501.pdf</url>
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      <volume>401</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <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>
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      <custom1>UR050</custom1>
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