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@ARTICLE{Rahman:203400,
      author       = {Rahman, M. and Sulis, M. and Kollet, Stefan},
      title        = {{T}he subsurface–land surface–atmosphere connection
                      under convective conditions},
      journal      = {Advances in water resources},
      volume       = {83},
      issn         = {0309-1708},
      address      = {Amsterdam [u.a.]},
      publisher    = {Elsevier Science},
      reportid     = {FZJ-2015-05343},
      pages        = {240 - 249},
      year         = {2015},
      abstract     = {The dynamics of the free groundwater table influence land
                      surface soil moisture and energy balance components, and are
                      therefore also linked to atmospheric processes. In this
                      study, the sensitivity of the atmosphere to groundwater
                      table dynamics induced heterogeneity in land surface
                      processes is examined under convective conditions. A fully
                      coupled subsurface–land surface–atmosphere model is
                      applied over a 150 km × 150 km study area located in
                      Western Germany and ensemble simulations are performed over
                      two convective precipitation events considering two separate
                      model configurations based on groundwater table dynamics.
                      Ensembles are generated by varying the model atmospheric
                      initial conditions following the prescribed ensemble
                      generation method by the German Weather Service in order to
                      account for the intrinsic, internal atmospheric variability.
                      The results demonstrate that especially under strong
                      convective conditions, groundwater table dynamics affect
                      atmospheric boundary layer height, convective available
                      potential energy, and precipitation via the coupling with
                      land surface soil moisture and energy fluxes. Thus, this
                      study suggests that systematic uncertainties may be
                      introduced to atmospheric simulations if groundwater table
                      dynamics are neglected in the model.},
      cin          = {IBG-3},
      ddc          = {550},
      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:000360192200021},
      doi          = {10.1016/j.advwatres.2015.06.003},
      url          = {https://juser.fz-juelich.de/record/203400},
}