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- W2254080600 abstract "The convolution integral which defines the output of a linear system can be directly integrated if the change in the variables between sampling points is assumed to be a step function, a linear segment, or part of a sliding polynomial. This enables calculation of the output in continuous time, not just at the sampling points. While the two data sets being convolved must each be sampled at equal time increments, the two increments need not be the algorithms for convolving two functions defined by data sets take on specialised forms when one of the functions is defined by an algebraic expression. Three cases considered here are the Clark and Cordery-Webb models, and the Muskingum routing equation. An interactive suit of computer programs has been developed for the convenient use of these models as well as the general convolution equation." @default.
- W2254080600 created "2016-06-24" @default.
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- W2254080600 date "1986-01-01" @default.
- W2254080600 modified "2023-09-26" @default.
- W2254080600 title "Calculating the Output from Linear Hydrologic Systems" @default.
- W2254080600 hasPublicationYear "1986" @default.
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