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1000 Titel
  • What controls the tail behaviour of flood series: rainfall or runoff generation?
1000 Autor/in
  1. Macdonald, Elena |
  2. Merz, Bruno |
  3. Guse, Björn |
  4. Nguyen, Viet Dung |
  5. Guan, Xiaoxiang |
  6. Vorogushyn, Sergiy |
1000 Verlag
  • Copernicus Publications
1000 Erscheinungsjahr 2024
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2024-02-21
1000 Erschienen in
1000 Quellenangabe
  • 28(4):833-850
1000 Copyrightjahr
  • 2024
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.5194/hess-28-833-2024 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:p>Abstract. Many observed time series of precipitation and streamflow show heavy-tail behaviour. For heavy-tailed distributions, the occurrence of extreme events has a higher probability than for distributions with an exponentially receding tail. If we neglect heavy-tail behaviour we might underestimate the magnitude of rarely observed, high-impact events. Robust estimation of upper-tail behaviour is often hindered by the limited length of observational records. Using long time series and a better understanding of the relevant process controls can help with achieving more robust tail estimations. Here, a simulation-based approach is used to analyse the effect of precipitation and runoff generation characteristics on the upper tail of flood peak distributions. Long, synthetic precipitation time series with different tail behaviour are produced by a stochastic weather generator. These are used to force a conceptual rainfall–runoff model. In addition, catchment characteristics linked to a threshold process in the runoff generation are varied between model runs. We characterize the upper-tail behaviour of the simulated precipitation and discharge time series with the shape parameter of the generalized extreme value (GEV) distribution. Our analysis shows that runoff generation can strongly modulate the tail behaviour of flood peak distributions. In particular, threshold processes in the runoff generation lead to heavier tails. Beyond a certain return period, the influence of catchment processes decreases and the tail of the rainfall distribution asymptotically governs the tail of the flood peak distribution. Beyond which return period this is the case depends on the catchment storage in relation to the mean annual rainfall amount. </jats:p>
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1000 Förderer
  1. Deutsche Forschungsgemeinschaft |
  2. China Scholarship Council |
  3. Bundesministerium für Bildung und Forschung |
1000 Fördernummer
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1000 Förderprogramm
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1000 Dateien
1000 Förderung
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    1000 Förderer Deutsche Forschungsgemeinschaft |
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    1000 Förderer China Scholarship Council |
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    1000 Fördernummer -
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    1000 Förderer Bundesministerium für Bildung und Forschung |
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1000 Objektart article
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1000 Erstellt am 2024-05-23T18:19:26.206+0200
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1000 Zuletzt bearbeitet 2024-05-27T11:07:19.626+0200
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