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@ARTICLE{Shrestha:857176,
      author       = {Shrestha, P. and Sulis, M. and Simmer, C. and Kollet, S.},
      title        = {{E}ffects of horizontal grid resolution on
                      evapotranspiration partitioning using {T}err{S}ys{MP}},
      journal      = {Journal of hydrology},
      volume       = {557},
      issn         = {0022-1694},
      address      = {Amsterdam [u.a.]},
      publisher    = {Elsevier},
      reportid     = {FZJ-2018-06413},
      pages        = {910 - 915},
      year         = {2018},
      abstract     = {Biotic leaf transpiration (T) and abiotic evaporation (E)
                      are the two major pathways by which water is transferred
                      from land surfaces to the atmosphere. Earth system models
                      simulating the terrestrial water, carbon and energy cycle
                      are required to reliably embed the role of soil and
                      vegetation processes in order to realistically reproduce
                      both fluxes including their relative contributions to total
                      evapotranspiration (ET). Earth system models are also being
                      used with increasing spatial resolutions to better simulate
                      the effects of surface heterogeneity on the regional water
                      and energy cycle and to realistically include effects of
                      subsurface lateral flow paths, which are expected to feed
                      back on the exchange fluxes and their partitioning in the
                      model.Using the hydrological component of the Terrestrial
                      Systems Modeling Platform (TerrSysMP), we examine the
                      uncertainty in the estimates of T/ET ratio due to horizontal
                      model grid resolution for a dry and wet year in the Inde
                      catchment (western Germany). The aggregation of topography
                      results in smoothing of slope magnitudes and the filtering
                      of small-scale convergence and divergence zones, which
                      directly impacts the surface-subsurface flow. Coarsening of
                      the grid resolution from 120 m to 960 m increased the
                      available soil moisture for ground evaporation, and
                      decreased T/ET ratio by about $5\%$ and $8\%$ for dry and
                      wet year respectively. The change in T/ET ratio was more
                      pronounced for agricultural crops compared to forested
                      areas, indicating a strong local control of vegetation on
                      the ground evaporation, affecting the domain average
                      statistics.},
      cin          = {IBG-3 / NIC},
      ddc          = {690},
      cid          = {I:(DE-Juel1)IBG-3-20101118 / I:(DE-Juel1)NIC-20090406},
      pnm          = {255 - Terrestrial Systems: From Observation to Prediction
                      (POF3-255) / Towards regional-scale groundwater-atmosphere
                      coupled climate simulations $(hbn33_20170501)$},
      pid          = {G:(DE-HGF)POF3-255 / $G:(DE-Juel1)hbn33_20170501$},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000425077300071},
      doi          = {10.1016/j.jhydrol.2018.01.024},
      url          = {https://juser.fz-juelich.de/record/857176},
}