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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Copernicus Publications
2008-12-01
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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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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 |
work_keys_str_mv |
AT agioia runoffthresholdsinderivedfloodfrequencydistributions AT viacobellis runoffthresholdsinderivedfloodfrequencydistributions AT smanfreda runoffthresholdsinderivedfloodfrequencydistributions AT mfiorentino runoffthresholdsinderivedfloodfrequencydistributions |
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