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@ARTICLE{MartnezGarca:155361,
      author       = {Martínez García, Gonzalo and Pachepsky, Yakov A. and
                      Vereecken, Harry},
      title        = {{E}ffect of soil hydraulic properties on the relationship
                      between the spatial mean and variability of soil moisture},
      journal      = {Journal of hydrology},
      volume       = {516},
      issn         = {0022-1694},
      address      = {Amsterdam [u.a.]},
      publisher    = {Elsevier},
      reportid     = {FZJ-2014-04530},
      pages        = {154 - 160},
      year         = {2014},
      abstract     = {Knowledge of spatial mean soil moisture and its variability
                      over time is needed in many environmental applications. We
                      analyzed dependencies of soil moisture variability on
                      average soil moisture contents in soils with and without
                      root water uptake using ensembles of non-stationary water
                      flow simulations by varying soil hydraulic properties under
                      different climatic conditions. We focused on the dry end of
                      the soil moisture range and found that the magnitude of soil
                      moisture variability was controlled by the interplay of soil
                      hydraulic properties and climate. The average moisture at
                      which the maximum variability occurred depended on soil
                      hydraulic properties and vegetation. A positive linear
                      relationship was observed between mean soil moisture and its
                      standard deviation and was controlled by the parameter
                      defining the shape of soil water retention curves and the
                      spatial variability of saturated hydraulic conductivity. The
                      influence of other controls, such as variable weather
                      patterns, topography or lateral flow processes needs to be
                      studied further to see if such relationship persists and
                      could be used for the inference of soil hydraulic properties
                      from the spatiotemporal variation in soil moisture.},
      cin          = {IBG-3},
      ddc          = {690},
      cid          = {I:(DE-Juel1)IBG-3-20101118},
      pnm          = {246 - Modelling and Monitoring Terrestrial Systems: Methods
                      and Technologies (POF2-246) / 255 - Terrestrial Systems:
                      From Observation to Prediction (POF3-255)},
      pid          = {G:(DE-HGF)POF2-246 / G:(DE-HGF)POF3-255},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000339036100014},
      doi          = {10.1016/j.jhydrol.2014.01.069},
      url          = {https://juser.fz-juelich.de/record/155361},
}