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@ARTICLE{Cornelissen:820921,
      author       = {Cornelissen, Thomas and Diekkrüger, Bernd and Bogena,
                      Heye},
      title        = {{U}sing {H}igh-{R}esolution {D}ata to {T}est {P}arameter
                      {S}ensitivity of the {D}istributed {H}ydrological {M}odel
                      {H}ydro{G}eo{S}phere},
      journal      = {Water},
      volume       = {8},
      number       = {5},
      issn         = {2073-4441},
      address      = {Basel},
      publisher    = {MDPI},
      reportid     = {FZJ-2016-06185},
      pages        = {202 -},
      year         = {2016},
      abstract     = {Parameterization of physically based and distributed
                      hydrological models for mesoscale catchments remains
                      challenging because the commonly available data base is
                      insufficient for calibration. In this paper, we parameterize
                      a mesoscale catchment for the distributed model
                      HydroGeoSphere by transferring evapotranspiration parameters
                      calibrated at a highly-equipped headwater catchment in
                      addition to literature data. Based on this parameterization,
                      the sensitivity of the mesoscale catchment to spatial
                      variability in land use, potential evapotranspiration and
                      precipitation and of the headwater catchment to mesoscale
                      soil and land use data was conducted. Simulations of the
                      mesoscale catchment with transferred parameters reproduced
                      daily discharge dynamics and monthly evapotranspiration of
                      grassland, deciduous and coniferous vegetation in a
                      satisfactory manner. Precipitation was the most sensitive
                      input data with respect to total runoff and peak flow rates,
                      while simulated evapotranspiration components and patterns
                      were most sensitive to spatially distributed land use
                      parameterization. At the headwater catchment, coarse soil
                      data resulted in a change in runoff generating processes
                      based on the interplay between higher wetness prior to a
                      rainfall event, enhanced groundwater level rise and
                      accordingly, lower transpiration rates. Our results indicate
                      that the direct transfer of parameters is a promising method
                      to benefit highly equipped simulations of the headwater
                      catchments},
      cin          = {IBG-3},
      ddc          = {690},
      cid          = {I:(DE-Juel1)IBG-3-20101118},
      pnm          = {255 - Terrestrial Systems: From Observation to Prediction
                      (POF3-255)},
      pid          = {G:(DE-HGF)POF3-255},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000377984300033},
      doi          = {10.3390/w8050202},
      url          = {https://juser.fz-juelich.de/record/820921},
}