An assessment of the spatial and temporal variability of certain factors that condition the susceptibility of soils to erosion, i.e. surface states of bare ground, vegetation and morphology is possible through remote sensing. This approach is greatly helped by the precise management and flexibility in the use of GIS systems. These assets should further the acceptance of remote sensing in the spatial modeling of hydraulic runoff and erosion.
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King et al. (1993) studied this question.