A simple alternative formulation of Hershfield's statistical method for est
imating probable maximum precipitation (PMP) is proposed. Specifically, it
is shown that the published Hershfield data do not support the hypothesis t
hat there exists a PMP as a physical upper limit, and therefore a purely pr
obabilistic treatment of the data is more consistent. In addition, using th
e same data set, it is shown that Hershfield's estimate of PMP may be obtai
ned using the generalized extreme value (GEV) distribution with shape param
eter given as a specified linear function of the average value of annual ma
ximum precipitation series and for return period of about 60,000 years. Thi
s formulation substitutes completely the standard empirical nomograph that
is used for the application of the method. The application of the method ca
n be improved when long series of local rainfall data are available that su
pport an accurate estimation of the shape parameter of the GEV distribution
.