The relationship between climate changes and floods frequency is of great interest for addressing the complex analysis on the hydrologic cycle evolution. In this context, this study aims to assess, by a preliminary investigation, the climate changes effects on the floods frequency in several basins of the upper Tiber River, whose area is ranging from 100 km2 to 300 km2. For that, a continuous hydrological model coupled with a stochastic generation of rainfall and temperature has been used. Therefore, a long synthetic series of discharge have been generated from which the annual maximum discharges have been taken-out and, hence, the flood frequency curves defined. For the stochastic generation of precipitation, the Neyman-Scott Rectangular Pulse model has been used, while for the synthetic generation of temperature, an ARIMA model with fractional differentiation has been applied. The time series of discharge have been assessed by applying a continuous hydrological model developed ad hoc for the investigated basins. The model structure has been inferred by investigating the effects of antecedent wetness conditions on the outlet response of several experimental basins located in Central Italy. The analysis proposed here compares the actual time series of precipitation and temperature and the perturbed ones by assuming two different future scenarios obtained by the Global Circulation Model HadCM3. Results showed that geo-morphological and land-use characteristics of basins might have a paramount role in the changing of floods frequency.

Analysis of Climate Change Effects on Floods Frequency Through a Continuous Hydrological Modelling

Brocca Luca;Camici Stefania;Tarpanelli Angelica;Melone Florisa;Moramarco Tommaso
2011

Abstract

The relationship between climate changes and floods frequency is of great interest for addressing the complex analysis on the hydrologic cycle evolution. In this context, this study aims to assess, by a preliminary investigation, the climate changes effects on the floods frequency in several basins of the upper Tiber River, whose area is ranging from 100 km2 to 300 km2. For that, a continuous hydrological model coupled with a stochastic generation of rainfall and temperature has been used. Therefore, a long synthetic series of discharge have been generated from which the annual maximum discharges have been taken-out and, hence, the flood frequency curves defined. For the stochastic generation of precipitation, the Neyman-Scott Rectangular Pulse model has been used, while for the synthetic generation of temperature, an ARIMA model with fractional differentiation has been applied. The time series of discharge have been assessed by applying a continuous hydrological model developed ad hoc for the investigated basins. The model structure has been inferred by investigating the effects of antecedent wetness conditions on the outlet response of several experimental basins located in Central Italy. The analysis proposed here compares the actual time series of precipitation and temperature and the perturbed ones by assuming two different future scenarios obtained by the Global Circulation Model HadCM3. Results showed that geo-morphological and land-use characteristics of basins might have a paramount role in the changing of floods frequency.
2011
978-94-007-1142-6
Climate change
Floods frequency
Continuous hydrological modelling
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/310912
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