2014
DOI: 10.5194/nhess-14-1819-2014
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Estimation of synthetic flood design hydrographs using a distributed rainfall–runoff model coupled with a copula-based single storm rainfall generator

Abstract: Abstract. In this paper a procedure to derive synthetic flood design hydrographs (SFDH) using a bivariate representation of rainfall forcing (rainfall duration and intensity) via copulas, which describes and models the correlation between two variables independently of the marginal laws involved, coupled with a distributed rainfall-runoff model, is presented. Rainfall-runoff modelling (R-R modelling) for estimating the hydrological response at the outlet of a catchment was performed by using a conceptual fully… Show more

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Cited by 43 publications
(35 citation statements)
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“…The idea to use Huff curves to generate an internal storm structure has also been adopted by Candela et al (2014). Given the 105-year time series at hand, empirical Huff curves can be obtained by partitioning each storm in the time series in e.g.…”
Section: Historical Time Series Characteristicsmentioning
confidence: 99%
“…The idea to use Huff curves to generate an internal storm structure has also been adopted by Candela et al (2014). Given the 105-year time series at hand, empirical Huff curves can be obtained by partitioning each storm in the time series in e.g.…”
Section: Historical Time Series Characteristicsmentioning
confidence: 99%
“…Candela et al (2014) applied a bivariate Archimedean copula-based distribution for characterising rainfall duration and intensity, in order to generate single synthetic rainfall events to be used as input in a conceptual fully distributed rainfall-runoff model based on the curve number method. The copula approach was then applied to the peak flow and hydrograph volume series of 5000 events synthetically generated from such a procedure, to obtain the flood design hydrograph related to a given joint return period.…”
Section: Introductionmentioning
confidence: 99%
“…In the relatively recent literature, there is a wide application of the copula functions to model the natural variability of hydrometeorological variables, ranging from rainfall (De Michele and Salvadori, 2003;Zhang and Singh, 2007;Balistrocchi and Bacchi, 2011;Singh and Zhang, 2007;Ariff et al, 2012) to floods (Aronica et al, 2012;Balistrocchi et al, 2014;Candela et al, 2014;Domeneghetti et al, 2013;Gräler et al, 2013;Ganguli and Reddy, 2013). …”
Section: Introductionmentioning
confidence: 99%