Regional frequency analysis of annual maximum flood data comprising 407 sta
tions from 11 countries of southern Africa is presented. Forty-one homogene
ous regions are identified. The L-moments of the observed data indicate tha
t the possible underlying frequency distributions are Pearson type 3 (P3),
lognormal 3-parameter (LN3), General Pareto (GPA) or General Extreme Value
(GEV). Simulation experiments for the selection of the most suitable flood
frequency procedure indicate that Pearson type 3/Probability Weighted Momen
ts (P3/PWM) and log-Pearson type 3/Method of Moments (LP3/MOM) are suitable
procedures for the region.