2013
DOI: 10.2166/nh.2013.243
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Spatial prediction of the runoff coefficient in Southern Peninsular Italy for the index flood estimation

Abstract: The runoff coefficient φ is a crucial parameter for the estimation of the mean value of annual maximum flood peak discharges in ungauged watersheds, where no direct measures are available. If the rational method is applied as a rainfall–runoff transformation model, the runoff coefficient accounts for all the hydrological losses, and it can be conceptually defined as the fraction of the total rainfall contributing to the flood peak response. In the present paper, focusing on the Southern Peninsular Italy, a reg… Show more

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Cited by 13 publications
(9 citation statements)
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“…The proposed approach highlights another complementary aspect related to the estimation of annual runoff along slope areas, which is particularly relevant for the management of surficial water resources. The calculated mean ARC values varying from 36 to 50 % can be approximately compared with those determined for Dinaric karst aquifers (Horvat and Rubinic, 2006) and some river basins of southern continental Italy (Del Giudice et al, 2013).…”
Section: Discussionmentioning
confidence: 77%
“…The proposed approach highlights another complementary aspect related to the estimation of annual runoff along slope areas, which is particularly relevant for the management of surficial water resources. The calculated mean ARC values varying from 36 to 50 % can be approximately compared with those determined for Dinaric karst aquifers (Horvat and Rubinic, 2006) and some river basins of southern continental Italy (Del Giudice et al, 2013).…”
Section: Discussionmentioning
confidence: 77%
“…Wang et al [50] developed a modified rational method for arid-region runoff estimation. Del Giudice et al [51] analyzed the spatial prediction of the runoff coefficient for flood index estimation and compared it with the rational method in Peninsular Italy.…”
Section: Modified Rational Methodsmentioning
confidence: 99%
“…The i-Tree Hydro model was calibrated to match the regional runoff ratio; no observed data were available for the four study site river basins, so runoff ratios were used. The initial soil parameter values were estimated as blend of hydrologic soil groups B and C, based on work of Del Giudice et al [26] and assigned the texture class silt loam for the i-Tree Hydro simulation. The Del Giudice et al [26] data were also used to estimate the runoff ratio for the river basins.…”
Section: Methodsmentioning
confidence: 99%
“…The initial soil parameter values were estimated as blend of hydrologic soil groups B and C, based on work of Del Giudice et al [26] and assigned the texture class silt loam for the i-Tree Hydro simulation. The Del Giudice et al [26] data were also used to estimate the runoff ratio for the river basins. The calibration exercises resulted in final parameter values for each river basin that were used to estimate the discharge during the 2015 year and the specific date of 11 August 2015.…”
Section: Methodsmentioning
confidence: 99%