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- W1999306656 abstract "Overland flow erosion has a significant role in determining the drainage properties of a land surface. Most physically based models of soil erosion over hillslopes use a constant value of critical shear stress τcr and soil erodibility Ct. The amount of soil loss predicted from hillslopes is very sensitive to these parameters. However, point-scale (or local-scale) measurements of these quantities exhibit variability over hillslopes. This paper presents a method for upscaling these values based on the distributions of τcr and Ct. Examples are considered for transient, one-dimensional flow under single storm events to demonstrate the spatiotemporal variation of the field-scale values of τcr and Ct for some realistic cases. These examples reinforced the need to account for spatial variability of parameters to make realistic predictions of soil loss through erosion by overland flow. The influence of spatial trend in the mean behavior of the critical shear stresses and soil erodibilities also is shown to have a significant impact on soil erosion from a hillslope." @default.
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- W1999306656 date "1998-03-01" @default.
- W1999306656 modified "2023-10-18" @default.
- W1999306656 title "Effective Erosion Parameters for Slopes with Spatially Varying Properties" @default.
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- W1999306656 doi "https://doi.org/10.1061/(asce)0733-9437(1998)124:2(81)" @default.
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