Hyetographs are essential to many hydrological designs. Many studies have s
hown that hyetographs are specific to storm types and durations. Recent wor
k presented evidence that dimensionless hyetographs are scale invariant. We
show that the simple scaling property of rainfall guarantees that the norm
alized rainfall rates of different storm durations are identically distribu
ted and propose a nonstationary Gauss-Markov model based on the annual maxi
mum events that arise from the dominant storm type. We derive the unique es
timators for the parameters of the Gauss-Markov model under two constraints
that: (a) the typical peak rainfall rate is preserved, and (b) the most li
kely hyetograph is obtained. One attractive feature of this model is that i
t allows translating hyetographs between storms of different durations. Two
examples illustrate our model.