Abstract
Risk can be estimated by the probability of exceedance of XT (flow with return period T). An accurate determination of XT with its confidence intervals is important in this context. We will consider estimation of XT using several methods in the case of the Pearson type 3 and log Pearson type 3 distributions.
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© 1991 Springer-Verlag Berlin Heidelberg
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Bobée, B., Ashkar, F., Roy, R., Perreault, L. (1991). Risk Analysis of Hydrological Data Using Gamma Family and Derived Distributions. In: Ganoulis, J. (eds) Water Resources Engineering Risk Assessment. NATO ASI Series, vol 29. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-76971-9_2
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DOI: https://doi.org/10.1007/978-3-642-76971-9_2
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