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  • Earth Resources and Remote Sensing  (1)
  • heterogeneity  (1)
  • unsaturated zone  (1)
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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Transport in porous media 3 (1988), S. 491-514 
    ISSN: 1573-1634
    Keywords: Review ; unsaturated zone ; analytical solution ; numerical model ; water ; Richards equation ; macroporosity ; heterogeneity ; spatial variability ; stochastic ; heat ; air
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Technology
    Notes: Abstract This paper reviews recent advances in analytical and numerical solution of problems of water flow through rigid soils in the unsaturated zone. The Richards model remains the most widely accepted and fertile framework for water flow analyses. More general formulations are reserved for the analysis of problems involving macroporosity, thermal effects, and air pressure effects. Many exact and approximate solutions have been derived for particular boundary value problems of homogeneous soils using methods such as quasi-linear analysis, Green-Ampt analysis, perturbation, and the kinematic wave approximation. Numerical simulators have become bigger and more accurate due to improvements in the areas of nonlinear solution procedures, mass conservation, computational efficiency, and computer hardware. Problems of natural heterogeneity have been addressed primarily through application of various stochastic methods to the Richards model. The stochastic formulations generally refute the concept of simple ‘equivalent’ homogeneous properties, but do themselves offer a certain limited potential for a predictive capability.
    Type of Medium: Electronic Resource
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  • 2
    Publication Date: 2019-07-17
    Description: Soil moisture anomalies dissipate over timescales that may span weeks to months. Characterizing the geographical and seasonal variations in these timescales can have important practical benefit; significant soil moisture "memory" allows long-lead forecasts of soil moisture, which have been found in recent studies to be essential for useful Ion--lead forecasts of precipitation in many regions. In this talk, we will present and compare the soil moisture timescales derived in two separate general circulation model (GCM) studies. Both studies employ multiple ensembles of short-term climate simulations. Timescales at a given point are effectively estimated by determining how quickly the soil moisture distribution generated in one ensemble of simulations (characterized by a unique set of initial soil moisture conditions) approaches that produced by another ensemble (characterized by a different set of initial soil moisture conditions). The talk will include a discussion of why the timescales produced by the two GCMs differ in some regions, and it will also describe the impact of soil moisture memory on simulated precipitation.
    Keywords: Earth Resources and Remote Sensing
    Type: Jan 09, 1999 - Jan 14, 1999; Long Beach, CA; United States
    Format: text
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