Regional frequency analysis of annual maximum flood data comprising 407 stations from 11 countries of southern Africa is presented. Forty-one homogeneous regions are identified. The L-moments of the observed data indicate that 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 Moments (P3/PWM) and log-Pearson type 3/Method of Moments (LP3/MOM) are suitable procedures for the region. © 2000 Taylor & Francis Group, LLC.
CITATION STYLE
MKHANDI, S. H., KACHROO, R. K., & GUNASEKARA, T. A. G. (2000). Flood frequency analysis of southern Africa: II. Identification of regional distributions. Hydrological Sciences Journal, 45(3), 449–464. https://doi.org/10.1080/02626660009492341
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