A technique for deriving an average event unit hydrograph from streamflow-only data for ephemeral quick-flow-dominant catchments
A technique is presented for empirical and parametric estimation of an average event unit hydrograph response curve solely from measured streamflow data for use in rainfall-runoff models with a focus on modelling flow for natural resource management. As the technique does not require rainfall data, the unit hydrograph can be derived solely from streamflow data at a temporal resolution appropriate for the response of the catchment. The response curves derived for a number of stations show a...[Show more]
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|Source:||Advances in Water Resources|
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