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@ARTICLE{Maxwell:203176,
      author       = {Maxwell, R. M. and Condon, L. E. and Kollet, Stefan},
      title        = {{A} high-resolution simulation of groundwater and surface
                      water over most of the continental {US} with the integrated
                      hydrologic model {P}ar{F}low v3},
      journal      = {Geoscientific model development},
      volume       = {8},
      number       = {3},
      issn         = {1991-9603},
      address      = {Katlenburg-Lindau},
      publisher    = {Copernicus},
      reportid     = {FZJ-2015-05181},
      pages        = {923 - 937},
      year         = {2015},
      abstract     = {Interactions between surface and groundwater systems are
                      well-established theoretically and observationally. While
                      numerical models that solve both surface and subsurface flow
                      equations in a single framework (matrix) are increasingly
                      being applied, computational limitations have restricted
                      their use to local and regional studies. Regional or
                      watershed-scale simulations have been effective tools for
                      understanding hydrologic processes; however, there are still
                      many questions, such as the adaptation of water resources to
                      anthropogenic stressors and climate variability, that can
                      only be answered across large spatial extents at high
                      resolution. In response to this grand challenge in
                      hydrology, we present the results of a parallel, integrated
                      hydrologic model simulating surface and subsurface flow at
                      high spatial resolution (1 km) over much of continental
                      North America (~ 6.3 M km2). These simulations provide
                      integrated predictions of hydrologic states and fluxes,
                      namely, water table depth and streamflow, at very large
                      scale and high resolution. The physics-based modeling
                      approach used here requires limited parameterizations and
                      relies only on more fundamental inputs such as topography,
                      hydrogeologic properties and climate forcing. Results are
                      compared to observations and provide mechanistic insight
                      into hydrologic process interaction. This study demonstrates
                      both the feasibility of continental-scale integrated models
                      and their utility for improving our understanding of
                      large-scale hydrologic systems; the combination of high
                      resolution and large spatial extent facilitates analysis of
                      scaling relationships using model outputs.},
      cin          = {IBG-3},
      ddc          = {910},
      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:000352160200026},
      doi          = {10.5194/gmd-8-923-2015},
      url          = {https://juser.fz-juelich.de/record/203176},
}