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The effects of our interventions on the physical model affect the water flow downstream outside of the model's boundaries, and similarly modeling water flow without considering surface runoff from outside the model results in underestimating the amount of water in the landscape.
Isohydric behavior of sagebrush indicates that well-known forest ecosystem models with greater gSR and −m can be used for modeling water, energy and carbon cycles from sagebrush and similar ecosystems.
This chapter presents a discussion of the principles and techniques for modeling water consumption and reuse, including how to handle complexity and to ensure model adequacy and sufficient precision.
Saturated hydraulic conductivity (Ks) is a key input parameter for modeling water flow in soils.
We discuss the advantages and disadvantages of using service-oriented computing for modeling water resource systems, and conclude with future work needed to advance the application of service-oriented computing for modeling water resource systems.
Modeling water velocities and depth for riverine aquatic habitat analysis requires fine-scale surveys of river bathymetry.
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In fact, models like PnET-II strongly rely on carbon allocation in modeling forest water yield and productivity in response to drought for Northeastern U.S. forests (Aber et al. 1995; Ollinger et al. 1997).
For modeling drinking water As exposures, we used the NHANES data to assess the timing and amounts of direct and indirect drinking water intake within a simulated person-day.
Modeling root water uptake within the macroscopic approach is usually done by introducing a sink term in the Richards equation.
Considered herein is a two-component Camassa Holm system modeling shallow water waves moving over a linear shear flow.
have been applied to multivariate modeling in water engineering.
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