Under the conditions of system linearity and stationarity of the precipitat
ion process we derive the hyetograph associated with any given flood discha
rge Q, using best linear unbiased estimation (BLUE) theory. The BLUE hyetog
raph depends explicitly on the correlation characteristics of the rainfall
process and the instantaneous unit hydrograph (IUH) of the basin. When the
correlation time of the rainfall process is short relative to the dispersio
n of the IUH, the shape of the BLUE hyetograph is the mirror image of the I
UH itself. In the opposite case the design hyetograph is the mirror image o
f the rainfall correlation function. The procedure is extended from lumped
to semidistributed and distributed basins. In the latter case we obtain sim
ultaneous design hyetographs for each subbasin or each site in the basin. T
he analytical findings and the possibility of regionalization are verified
using synthetic and recorded rainfall time series, with excellent agreement
in both cases. Because of its simplicity, robustness, and theoretical basi
s the proposed procedure should be appealing for practical use, particularl
y when not only the peak but the entire flood hydrograph is required.