Runoff thresholds in derived flood frequency distributions

In general, different mechanisms may be identified as responsible of runoff generation during ordinary events or extraordinary events at the basin scale. In a simplified scheme these mechanisms may be represented by different runoff thresholds. In this context, the derived flood frequency model, bas...

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Main Authors: A. Gioia, V. Iacobellis, S. Manfreda, M. Fiorentino
Format: Article
Language:English
Published: Copernicus Publications 2008-12-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/12/1295/2008/hess-12-1295-2008.pdf
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spelling doaj-57cf010359684d58971c0b763909be902020-11-24T21:35:40ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382008-12-0112612951307Runoff thresholds in derived flood frequency distributionsA. GioiaV. IacobellisS. ManfredaM. FiorentinoIn general, different mechanisms may be identified as responsible of runoff generation during ordinary events or extraordinary events at the basin scale. In a simplified scheme these mechanisms may be represented by different runoff thresholds. In this context, the derived flood frequency model, based on the effect of partial contributing areas on peak flow, proposed by Iacobellis and Fiorentino (2000), was generalized by providing a new formulation of the derived distribution where two runoff components are explicitly considered. The model was tested on a group of basins in Southern Italy characterized by annual maximum flood distributions highly skewed. The application of the proposed model provided good results in terms of descriptive ability. Model parameters were also found to be well correlated with geomorphological basin descriptors. Two different threshold mechanisms, associated respectively to ordinary and extraordinary events, were identified. In fact, we found that ordinary floods are mostly due to rainfall events exceeding a threshold infiltration rate in a small source area, while the so-called outlier events, responsible of the high skewness of flood distributions, are triggered when severe rainfalls exceed a threshold storage in a large portion of the basin. http://www.hydrol-earth-syst-sci.net/12/1295/2008/hess-12-1295-2008.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. Gioia
V. Iacobellis
S. Manfreda
M. Fiorentino
spellingShingle A. Gioia
V. Iacobellis
S. Manfreda
M. Fiorentino
Runoff thresholds in derived flood frequency distributions
Hydrology and Earth System Sciences
author_facet A. Gioia
V. Iacobellis
S. Manfreda
M. Fiorentino
author_sort A. Gioia
title Runoff thresholds in derived flood frequency distributions
title_short Runoff thresholds in derived flood frequency distributions
title_full Runoff thresholds in derived flood frequency distributions
title_fullStr Runoff thresholds in derived flood frequency distributions
title_full_unstemmed Runoff thresholds in derived flood frequency distributions
title_sort runoff thresholds in derived flood frequency distributions
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2008-12-01
description In general, different mechanisms may be identified as responsible of runoff generation during ordinary events or extraordinary events at the basin scale. In a simplified scheme these mechanisms may be represented by different runoff thresholds. In this context, the derived flood frequency model, based on the effect of partial contributing areas on peak flow, proposed by Iacobellis and Fiorentino (2000), was generalized by providing a new formulation of the derived distribution where two runoff components are explicitly considered. The model was tested on a group of basins in Southern Italy characterized by annual maximum flood distributions highly skewed. The application of the proposed model provided good results in terms of descriptive ability. Model parameters were also found to be well correlated with geomorphological basin descriptors. Two different threshold mechanisms, associated respectively to ordinary and extraordinary events, were identified. In fact, we found that ordinary floods are mostly due to rainfall events exceeding a threshold infiltration rate in a small source area, while the so-called outlier events, responsible of the high skewness of flood distributions, are triggered when severe rainfalls exceed a threshold storage in a large portion of the basin.
url http://www.hydrol-earth-syst-sci.net/12/1295/2008/hess-12-1295-2008.pdf
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AT viacobellis runoffthresholdsinderivedfloodfrequencydistributions
AT smanfreda runoffthresholdsinderivedfloodfrequencydistributions
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