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- W1995662140 abstract "A two‐dimensional, finite difference model of saturated subsurface hillslope flow, capable of handling varied topography, is developed. The model uses rainfall, elevation data, saturated conductivities, and available soil porosity to predict saturated thicknesses in time and space over the hillslope. The model is tested against piezometric data collected in a steep hillslope hollow in the Cascade Range of Washington state during the winter wet season. The model closely tracks the timing and magnitude of piezometric response." @default.
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- W1995662140 modified "2023-09-26" @default.
- W1995662140 title "A model of transient, topographically driven, saturated subsurface flow" @default.
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- W1995662140 doi "https://doi.org/10.1029/91wr02923" @default.
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