The unit hydrograph is a common tool in hydraulic design. Used correct
ly, it allows a design engineer to estimate a runoff hydrograph from a
drainage basin given a rainfall event. The typical method for estimat
ing a unit hydrograph for a gaged watershed is by deconvolution. Howev
er, distinct storms produce different unit hydrographs for a single wa
tershed. Consequently, a design engineer usually develops a composite,
or average, unit hydrograph based on several recorded storm events. C
ommon methods for estimating this composite unit hydrograph include cu
rve fitting, simple aggregation, and multistorm optimization technique
s. This paper introduces a new method to perform aggregation of unit h
ydrographs. The method is an extension to the simple averaging techniq
ue, in which prior to averaging, the individual unit hydrograph time o
rdinates are normalized with respect to the average time to peak. The
normalization method is compared to a simple averaging technique and t
wo multistorm aggregation techniques at six rural watersheds in Alabam
a. The results indicate that on average the normalization method predi
cts runoff nearly as accurately as the multistorm techniques, and disp
lays improvement for 60 percent of the storms tested when compared wit
h the simple averaging technique.