dot
Detailansicht
Katalogkarte GBA
Katalogkarte ISBD
Suche präzisieren
Drucken
Download RIS
Hier klicken, um den Treffer aus der Auswahl zu entfernen
Titel A peaks-over-threshold model for floods with zero-inflated Poisson arrivals
VerfasserIn Artur Tiago Silva, Maria Manuela Portela, Mauro Naghettini
Konferenz EGU General Assembly 2013
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 15 (2013)
Datensatznummer 250072065
 
Zusammenfassung
The peaks-over-threshold (POT) model for hydrological extremes with Poisson arrivals and Generalized Pareto (GP) distributed exceedances remains a popular and useful tool for modelling hydrologic extremes. The use of the Poisson-GP model for flood frequency analysis requires the validation of the Poisson hypothesis: that the distribution of the annual number of flood events may be described by a Poisson distribution. Such hypothesis is not always valid in practical applications. The present study concerns the use of an alternative distribution for modelling the annual number of floods - the Zero-Inflated Poisson (ZIP) distribution with two parameters. A ZIP-GP model for flood frequency analysis is proposed. This model is less restrictive than the Poisson-GP model since it allows for a more accurate description of the occurrence process in a POT framework if the fraction of years with no exceedances is significantly higher than the theoretical density at zero of the Poisson distribution. Applications of the ZIP-GP model to flood data from Northern Portugal and the evaluation of its performance relative to the Poisson-GP model, including assessments of quantile uncertainty, are presented. The results show that, overall, the ZIP-GP model outperforms the Poisson-GP model, especially for lower quantiles, hence the ZIP distribution is a valid alternative to the Poisson distribution for modelling the annual occurrence counts of peaks in a POT approach for flood frequency analysis. Moreover, despite the ZIP having one more parameter, there is no increment in uncertainty for higher quantiles of the ZIP-GP model.