ON THE DERIVED FLOOD FREQUENCY DISTRIBUTION: ANALYTICAL FORMULATION AND THE INFLUENCE OF ANTECEDENT SOIL MOISTURE CONDITION

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dc.contributor.author Michele C.D.
dc.contributor.author Salvadori G.
dc.date.accessioned 2021-04-17T00:44:01Z
dc.date.available 2021-04-17T00:44:01Z
dc.date.issued 2002
dc.identifier https://www.elibrary.ru/item.asp?id=1064609
dc.identifier.citation Journal of Hydrology, 2002, 262, 1-4, 245-258
dc.identifier.issn 0022-1694
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/27957
dc.description.abstract In this paper we present an analytical formulation of the derived distribution of peak flood and maximum annual peak flood, starting from a simplified description of rainfall and surface runoff processes, and we show how such a distribution is useful in practical applications. The assumptions on rainfall dynamics include the hypotheses that the maximum storm depth has a Generalized Pareto distribution, and that the temporal variability of rainfall depth in a storm can be described via power-law relationships. The SCS-CN model is used to describe the soil response, and a lumped model is adopted to transform the rainfall excess into peak flood; in particular, we analyse the influence of antecedent soil moisture condition on the flood frequency distribution. We then calculate the analytical expressions of the derived distributions of peak flood and maximum annual peak flood. Finally, practical case studies are presented and discussed.
dc.subject ANTECEDENT SOIL MOISTURE CONDITION
dc.subject DERIVED DISTRIBUTION
dc.subject EXTREME EVENT
dc.subject GENERALIZED PARETO
dc.subject MAXIMUM ANNUAL PEAK FLOOD
dc.subject PEAK FLOOD
dc.title ON THE DERIVED FLOOD FREQUENCY DISTRIBUTION: ANALYTICAL FORMULATION AND THE INFLUENCE OF ANTECEDENT SOIL MOISTURE CONDITION
dc.type Статья


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