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A Simple Flood Hydrograph Model for Urban Catchments

MC Bufill, MJ Boyd

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Abstract

Study of rainfall and runoff depths, and runoff hydrographs on 16 urban catchments, has indicated that runoff from pervious and impervious areas should be modelled separately. For small storms, runoff comes predominantly from impervious surfaces, while for the larger less frequent storms, runoff is generated on both pervious and impervious surfaces. The lag parameter for impervious runoff can be successfully estimated from hydrograph recessions. A parallel reservoir model is suggested as an adequate model for urban catchment hydrographs.

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What this paper is about

Study of rainfall and runoff depths, and runoff hydrographs on 16 urban catchments, has indicated that runoff from pervious and impervious areas should be modelled separately. For small storms, runoff comes predominantly from impervious surfaces, while for the larger less frequent storms, runoff is generated on both pervious and impervious surfaces. The lag parameter for impervious runoff can be successfully estimated from hydrograph recessions. A parallel reservoir model is suggested as an adequate model for urban catchment hydrographs.

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Available abstract

Study of rainfall and runoff depths, and runoff hydrographs on 16 urban catchments, has indicated that runoff from pervious and impervious areas should be modelled separately. For small storms, runoff comes predominantly from impervious surfaces, while for the larger less frequent storms, runoff is generated on both pervious and impervious surfaces. The lag parameter for impervious runoff can be successfully estimated from hydrograph recessions. A parallel reservoir model is suggested as an adequate model for urban catchment hydrographs.

Key concepts: Impervious surface, Hydrograph, Surface runoff, Runoff model, Hydrology (agriculture), Environmental science, Runoff curve number, Storm

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