% IMPORTANT: The following is UTF-8 encoded.  This means that in the presence
% of non-ASCII characters, it will not work with BibTeX 0.99 or older.
% Instead, you should use an up-to-date BibTeX implementation like “bibtex8” or
% “biber”.

@BOOK{Bogena:45087,
      author       = {Bogena, Heye and Herbst, Michael and Hake,
                      Jürgen-Friedrich and Kunkel, Ralf and Montzka, Carsten and
                      Pütz, Thomas and Vereecken, Harry and Wendland, Frank},
      title        = {{MOSYRUR} - {W}ater balance analysis in the {R}ur basin},
      volume       = {52},
      address      = {Jülich},
      publisher    = {Forschungszentrum Jülich GmbH Zentralbibliothek, Verlag},
      reportid     = {PreJuSER-45087},
      isbn         = {3-89336-385-8},
      series       = {Schriften des Forschungszentrums Jülich. Reihe Umwelt /
                      Environment},
      pages        = {155 S.},
      year         = {2005},
      note         = {Record converted from VDB: 12.11.2012},
      abstract     = {In this report the current results of the research
                      activities in the MOSYRUR project are summarized. The
                      targets of the first project phase (2002-2004) were the
                      analysis of the quantitative status of the water resources
                      in the catchment of the Rur ($\sim$2350 km$^{2}$) and the
                      indication of the water balance at different scales. Process
                      orientated investigations and simulations were performed at
                      the small meso-scale test area "Zwischenscholle" (20
                      km$^{2}$) using the TRACE model. For the model application
                      the potential evapotranspiration was calculated,
                      Pedotransfer functions were utilized in order to derive the
                      soil hydraulic properties and borehole measurements of
                      groundwater levels were spatially and temporally
                      interpolated in order to define the vertical boundary
                      conditions. A one-dimensional and a three-dimensional TRACE
                      application were performed for the period 1.12.1983 to
                      31.11.1993. The one-dimensional TRACE application was
                      validated using a lysimeter experiment dataset spanning the
                      period from 25.11.1988 to 13.8.1990. The actual
                      evapotranspiration is slightly underestimated, while the
                      amount of drainage is slightly overestimated. Nevertheless
                      the calculated model performance measures indicate that all
                      relevant processes and state variables (evapotranspiration,
                      drainage and soil moisture) are well described. The measured
                      actual evapotranspiration for the whole modelling period is
                      990 mm, whereas TRACE calculates an amount of 977 mm. The
                      deviation between the measured drainage amount of 158 mm and
                      the amount predicted with TRACE (163 mm) is equal to an
                      error of 3.4 \%. A decrease in soil moisture during the
                      first spring at 85 cm depth is not that well reproduced,
                      which might be attributed to a plant compensation mechanism.
                      Probably the plant adapts to the low soil moisture near the
                      surface by taking out more water at deeper soil layers. The
                      validation of the three-dimensional TRACE application showed
                      that the groundwater levels measured at the field scale are,
                      basically, well reproduced. Wells were selected, which are
                      located rather in the middle of the test area than close to
                      the boundary, since the model results and measured heads are
                      supposed to be very similar near the boundary, where the
                      measurements are used for the imposed boundary condition.
                      The RMSE of these wells ranges between 0.33 and 0.68, which
                      is adequate since no calibration of the model was carried
                      out. The large-scaled GIS-supported GROWA model was applied
                      for balancing water components at the catchment scale . For
                      the model application datasets were used that were mainly
                      provided by the geological survey of NRW and the [...]},
      cin          = {STE / ICG-IV},
      ddc          = {333.7},
      cid          = {I:(DE-Juel1)VDB64 / I:(DE-Juel1)VDB50},
      pnm          = {Systemforschung; Technik, Umwelt, Gesellschaft / Chemie und
                      Dynamik der Geo-Biosphäre},
      pid          = {G:(DE-Juel1)FUEK258 / G:(DE-Juel1)FUEK257},
      typ          = {PUB:(DE-HGF)3},
      url          = {https://juser.fz-juelich.de/record/45087},
}