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    Propagating Subsurface Uncertainty to the Atmosphere Using Fully Coupled Stochastic Simulations 

    Source: Journal of Hydrometeorology:;2011:;Volume( 012 ):;issue: 004:;page 690
    Author(s): Williams, John L.; Maxwell, Reed M.
    Publisher: American Meteorological Society
    Abstract: eedbacks between the land surface and the atmosphere, manifested as mass and energy fluxes, are strongly correlated with soil moisture, making soil moisture an important factor in land?atmosphere interactions. It is shown ...
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    Development of a Coupled Land Surface and Groundwater Model 

    Source: Journal of Hydrometeorology:;2005:;Volume( 006 ):;issue: 003:;page 233
    Author(s): Maxwell, Reed M.; Miller, Norman L.
    Publisher: American Meteorological Society
    Abstract: Traditional land surface models (LSMs) used for numerical weather simulation, climate projection, and as inputs to water management decision support systems, do not treat the LSM lower boundary in a fully process-based ...
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    Effects of Water-Table Configuration on the Planetary Boundary Layer over the San Joaquin River Watershed, California 

    Source: Journal of Hydrometeorology:;2017:;Volume( 018 ):;issue: 005:;page 1471
    Author(s): Gilbert, James M.; Maxwell, Reed M.; Gochis, David J.
    Publisher: American Meteorological Society
    Abstract: he boundary layer, land surface, and subsurface are important coevolving components of hydrologic systems. While previous studies have examined the connections between soil moisture, groundwater, and the atmosphere, the ...
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    Exploring the Sensitivity of Photosynthesis and Stomatal Resistance Parameters in a Land Surface Model 

    Source: Journal of Hydrometeorology:;2017:;Volume( 018 ):;issue: 003:;page 897
    Author(s): Jefferson, Jennifer L.; Maxwell, Reed M.; Constantine, Paul G.
    Publisher: American Meteorological Society
    Abstract: and surface models, like the Common Land Model component of the ParFlow integrated hydrologic model (PF-CLM), are used to estimate transpiration from vegetated surfaces. Transpiration rates quantify how much water moves ...
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    Coupling Groundwater, Vegetation, and Atmospheric Processes: A Comparison of Two Integrated Models 

    Source: Journal of Hydrometeorology:;2017:;Volume( 018 ):;issue: 005:;page 1489
    Author(s): Sulis, Mauro; Williams, John L.; Shrestha, Prabhakar; Diederich, Malte; Simmer, Clemens; Kollet, Stefan J.; Maxwell, Reed M.
    Publisher: American Meteorological Society
    Abstract: his study compares two modeling platforms, ParFlow.WRF (PF.WRF) and the Terrestrial Systems Modeling Platform (TerrSysMP), with a common 3D integrated surface?groundwater model to examine the variability in simulated ...
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    Development of a Coupled Groundwater–Atmosphere Model 

    Source: Monthly Weather Review:;2010:;volume( 139 ):;issue: 001:;page 96
    Author(s): Maxwell, Reed M.; Lundquist, Julie K.; Mirocha, Jeffrey D.; Smith, Steven G.; Woodward, Carol S.; Tompson, Andrew F. B.
    Publisher: American Meteorological Society
    Abstract: Complete models of the hydrologic cycle have gained recent attention as research has shown interdependence between the coupled land and energy balance of the subsurface, land surface, and lower atmosphere. PF.WRF is a new ...
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