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This document discusses the calculation of a unit hydrograph (HU) and hydrograph (S-curve) from observed rainfall and flow data. It shows the HU calculated for a 12-hour effective rainfall and then uses this to generate the S-curve by successive shifts of the HU values at 12-hour intervals. It then takes the S-curve and shifts it by 24 hours to derive a new 24-hour HU, demonstrating how the unit hydrograph method can be used to model watershed response at different time scales.

Author

Nataly CP

Language

EN