Simple scaling theory explains the spatial variability of peak flow pr
ocesses by their indexation on a set of scale parameters, such as the
size of drainage basins. On this basis, a regional analysis can be con
ducted to construct a unique growth curve. However, a drawback of the
simple scaling approach is that it assumes that the coefficients of Va
riation of peak flow distributions are identical throughout a region.
Although empirical data might display statistical properties which cor
respond to simple scaling assumptions, the coefficient of variation of
flood peaks depends on drainage area. We discuss this fact here and w
e suggest using the empirical Bayes method to take into account this r
egional variation of the coefficient of variation. The advantage of us
ing an empirical Bayes analysis subsequent to simple scaling modeling
is illustrated using a set of 109 flood series from the Province of On
tario, Canada.