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@ARTICLE{Shrestha:279773,
      author       = {Shrestha, P. and Sulis, M. and Simmer, C. and Kollet, S.},
      title        = {{I}mpacts of grid resolution on surface energy fluxes
                      simulated with an integrated surface-groundwater flow model},
      journal      = {Hydrology and earth system sciences},
      volume       = {19},
      number       = {10},
      issn         = {1607-7938},
      address      = {Katlenburg-Lindau},
      publisher    = {EGU},
      reportid     = {FZJ-2015-07655},
      pages        = {4317 - 4326},
      year         = {2015},
      abstract     = {The hydrological component of the Terrestrial Systems
                      Modeling Platform (TerrSysMP), which includes integrated
                      surface-groundwater flow, was used to investigate the grid
                      resolution dependence of simulated soil moisture, soil
                      temperature, and surface energy fluxes over a sub-catchment
                      of the Rur, Germany. The investigation was motivated by the
                      recent developments of new earth system models, which
                      include 3-D physically based groundwater models for the
                      coupling of land–atmosphere interaction and subsurface
                      hydrodynamics. Our findings suggest that for grid
                      resolutions between 100 and 1000 m, the non-local controls
                      of soil moisture are highly grid resolution dependent. Local
                      vegetation, however, strongly modulates the scaling
                      behavior, especially for surface fluxes and soil
                      temperature, which depends on the radiative transfer
                      property of the canopy. This study also shows that for grid
                      resolutions above a few 100 m, the variation of spatial and
                      temporal patterns of sensible and latent heat fluxes may
                      significantly affect the resulting atmospheric mesoscale
                      circulation and boundary layer evolution in coupled runs.},
      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:000364327800018},
      doi          = {10.5194/hess-19-4317-2015},
      url          = {https://juser.fz-juelich.de/record/279773},
}