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@ARTICLE{Shrestha:171936,
      author       = {Shrestha, P. and Sulis, M. and Masbou, M. and Kollet, S.
                      and Simmer, C.},
      title        = {{A} {S}cale-{C}onsistent {T}errestrial {S}ystems {M}odeling
                      {P}latform {B}ased on {COSMO}, {CLM}, and {P}ar{F}low},
      journal      = {Monthly weather review},
      volume       = {142},
      number       = {9},
      issn         = {1520-0493},
      address      = {Washington, DC [u.a.]},
      publisher    = {AMS87486},
      reportid     = {FZJ-2014-05490},
      pages        = {3466 - 3483},
      year         = {2014},
      abstract     = {A highly modular and scale-consistent Terrestrial Systems
                      Modeling Platform (TerrSysMP) is presented. The modeling
                      platform consists of an atmospheric model (Consortium for
                      Small-Scale Modeling; COSMO), a land surface model (the NCAR
                      Community Land Model, version 3.5; CLM3.5), and a 3D
                      variably saturated groundwater flow model (ParFlow). An
                      external coupler (Ocean Atmosphere Sea Ice Soil, version
                      3.0; OASIS3) with multiple executable approaches is employed
                      to couple the three independently developed component
                      models, which intrinsically allows for a separation of
                      temporal–spatial modeling scales and the coupling
                      frequencies between the component models.Idealized TerrSysMP
                      simulations are presented, which focus on the interaction of
                      key hydrologic processes, like runoff production (excess
                      rainfall and saturation) at different hydrological modeling
                      scales and the drawdown of the water table through
                      groundwater pumping, with processes in the atmospheric
                      boundary layer. The results show a strong linkage between
                      integrated surface–groundwater dynamics, biogeophysical
                      processes, and boundary layer evolution. The use of the
                      mosaic approach for the hydrological component model (to
                      resolve subgrid-scale topography) impacts simulated runoff
                      production, soil moisture redistribution, and boundary layer
                      evolution, which demonstrates the importance of hydrological
                      modeling scales and thus the advantages of the coupling
                      approach used in this study.Real data simulations were
                      carried out with TerrSysMP over the Rur catchment in
                      Germany. The inclusion of the integrated
                      surface–groundwater flow model results in systematic
                      patterns in the root zone soil moisture, which influence
                      exchange flux distributions and the ensuing atmospheric
                      boundary layer development. In a first comparison to
                      observations, the 3D model compared to the 1D model shows
                      slightly improved predictions of surface fluxes and a strong
                      sensitivity to the initial soil moisture content.},
      cin          = {IBG-3},
      ddc          = {550},
      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:000341171100024},
      doi          = {10.1175/MWR-D-14-00029.1},
      url          = {https://juser.fz-juelich.de/record/171936},
}