% 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”.

@ARTICLE{Vanderborght:12520,
      author       = {Vanderborght, J. and Graf, A. and Steenpass, C. and
                      Scharnagl, B. and Prolingheuer, N. and Herbst, M. and
                      Hendricks-Franssen, H.-J. and Vereecken, H.},
      title        = {{W}ithin-{F}ield {V}ariability of {B}are {S}oil
                      {E}vaporation {D}erived from {E}ddy {C}ovariance
                      {M}easurements},
      journal      = {Vadose zone journal},
      volume       = {9},
      issn         = {1539-1663},
      address      = {Madison, Wis.},
      publisher    = {SSSA},
      reportid     = {PreJuSER-12520},
      pages        = {943-954},
      year         = {2010},
      note         = {This research was supported by the German Research
                      Foundation DFG (Transregional Collaborative Research Centre
                      32-Patterns in Soil-Vegetation-Atmosphere Systems:
                      Monitoring, modelling and data assimilation). We thank
                      Marius Schmidt and Karl Schneider from the University of
                      Cologne for providing meteorologic data from the Selhausen
                      test site and Axel Knaps for providing us with meteorologic
                      data from the Forschungszentrum Julich. A. Graf would like
                      to thank the DFG for funding through the project GR 2687/3-1
                      "Links between local scale and catchment scale measurements
                      and modelling of gas exchange processes over land
                      surfaces."},
      abstract     = {Bare soil evaporation was measured with the eddy-covariance
                      method at the Selhausen field site. The site has a distinct
                      gradient in soil texture, with a considerably higher stone
                      content at the upper part of the field. We investigated the
                      effect of different soil properties in the upper and lower
                      parts of the field on evaporation using eddy covariance (EC)
                      measurements that were combined with a footprint model.
                      Because only one EC station was available, simultaneous
                      evaporation measurements from the two field parts were not
                      available. Therefore, measurements were put into the context
                      of meteorologic and soil hydrologic conditions. Meteorologic
                      conditions were represented by the potential evaporation,
                      i.e., the maximum evaporation that is determined by the
                      energy available for evaporation. The influence of
                      precipitation and soil hydrologic conditions on the actual
                      evaporation rate was represented by a simple soil
                      evaporation model. The amount of water that could be
                      evaporated at the potential rate from the lower part of the
                      field was found to be large and considerably larger than
                      from the upper part of the field. The difference in
                      evaporation led to threefold larger predicted percolation or
                      runoff in the upper than the lower part of the field.
                      Simulations using the Richards equation were able to
                      reproduce the differences in evaporation between the lower
                      and upper parts of the field and relate them to the
                      different groundwater table depths in the two parts of the
                      field.},
      keywords     = {J (WoSType)},
      cin          = {IBG-3 / JARA-HPC},
      ddc          = {550},
      cid          = {I:(DE-Juel1)IBG-3-20101118 / $I:(DE-82)080012_20140620$},
      pnm          = {Terrestrische Umwelt},
      pid          = {G:(DE-Juel1)FUEK407},
      shelfmark    = {Environmental Sciences / Soil Science / Water Resources},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000287739800013},
      doi          = {10.2136/vzj2009.0159},
      url          = {https://juser.fz-juelich.de/record/12520},
}