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- W1966129211 abstract "A nonlinear mathematical model, starting with the integral of an infiltration capacity function, is developed to analytically equate the difference between rainfall and runoff to hydrologie variables. Only the three independent variables—storm rainfall, duration, and soil moisture—are used, and an equation is evolved in which the identity of the coefficients is kept intact and unusually good statistical control is maintained. The coefficients of the equation appear to be stable over a range of watershed sizes and conditions. The equation strongly indicates that runoff usually originates from a small, but relatively consistent, part of the watershed. The function can be manipulated to show a ‘function of apparent watershed infiltration capacity’ This function characterizes the infiltration capacity of that portion contributing to runoff, on the average, and should prove to be a useful infiltration capacity index with which watersheds can be compared. The equation itself provides insight into why in situ measurements of infiltration capacity seldom agree with the capacity determined from rainfall-runoff data. It also indicates why storm runoff frequently is not linear with respect to causative factors." @default.
- W1966129211 created "2016-06-24" @default.
- W1966129211 creator A5077395463 @default.
- W1966129211 date "1964-04-15" @default.
- W1966129211 modified "2023-10-18" @default.
- W1966129211 title "What is watershed runoff?" @default.
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- W1966129211 doi "https://doi.org/10.1029/jz069i008p01541" @default.
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