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@ARTICLE{Belleflamme:1007830,
      author       = {Belleflamme, Alexandre and Görgen, Klaus and Wagner,
                      Niklas and Kollet, Stefan and Bathiany, Sebastian and El
                      Zohbi, Juliane and Rechid, Diana and Vanderborght, Jan and
                      Vereecken, Harry},
      title        = {{H}ydrological forecasting at impact scale: the integrated
                      {P}ar{F}low hydrological model at 0.6 km for climate
                      resilient water resource management over {G}ermany},
      journal      = {Frontiers in water},
      volume       = {5},
      issn         = {2624-9375},
      address      = {Lausanne},
      publisher    = {Frontiers Media},
      reportid     = {FZJ-2023-02215},
      pages        = {1183642},
      year         = {2023},
      abstract     = {In the context of the repeated droughts that have affected
                      central Europe over the last years (2018–2020, 2022),
                      climate-resilient management of water resources, based on
                      timely information about the current state of the
                      terrestrial water cycle and forecasts of its evolution, has
                      gained an increasing importance. To achieve this, we propose
                      a new setup for simulations of the terrestrial water cycle
                      using the integrated hydrological model ParFlow/CLM at high
                      spatial and temporal resolution (i.e., 0.611 km, hourly time
                      step) over Germany and the neighboring regions. We show that
                      this setup can be used as a basis for a monitoring and
                      forecasting system that aims to provide stakeholders from
                      many sectors, but especially agriculture, with diagnostics
                      and indicators highlighting different aspects of subsurface
                      water states and fluxes, such as subsurface water storage,
                      seepage water, capillary rise, or fraction of plant
                      available water for different (root-)depths. The validation
                      of the new simulation setup with observation-based data
                      monthly over the period 2011–2020 yields good results for
                      all major components of the terrestrial water cycle analyzed
                      here, i.e., volumetric soil moisture, evapotranspiration,
                      water table depth, and river discharge. As this setup relies
                      on a standardized grid definition and recent globally
                      available static fields and parameters (e.g., topography,
                      soil hydraulic properties, land cover), the workflow could
                      easily be transferred to many regions of the Earth,
                      including sparsely gauged regions, since ParFlow/CLM does
                      not require calibration.},
      cin          = {IBG-3},
      ddc          = {333.7},
      cid          = {I:(DE-Juel1)IBG-3-20101118},
      pnm          = {2173 - Agro-biogeosystems: controls, feedbacks and impact
                      (POF4-217)},
      pid          = {G:(DE-HGF)POF4-2173},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:001007969000001},
      doi          = {10.3389/frwa.2023.1183642},
      url          = {https://juser.fz-juelich.de/record/1007830},
}