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Nonlinear instantaneous unit-hydrograph theory
Analysis of hyetographs and hydrographs for various storms over 6 drainage basins indicates definite relationship between time of concentration and channel storage discharge factor, and instantaneous equivalent rainfall excess; procedures for analysis of data to establish relations between parameters and rainfall excess, and use of established relations to derive surface runoff hydrograph from given effective hyetograph are explained and supplemented by examples.
Nonlinear instantaneous unit-hydrograph theory
Analysis of hyetographs and hydrographs for various storms over 6 drainage basins indicates definite relationship between time of concentration and channel storage discharge factor, and instantaneous equivalent rainfall excess; procedures for analysis of data to establish relations between parameters and rainfall excess, and use of established relations to derive surface runoff hydrograph from given effective hyetograph are explained and supplemented by examples.
Nonlinear instantaneous unit-hydrograph theory
ASCE -- Proc (J Hydraulics Div)
Singh, K.P. (author)
1964
35 pages
Article (Journal)
English
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