2013
DOI: 10.1016/j.jhydrol.2013.10.020
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Generating synthetic time series of springs discharge in relation to standardized precipitation indices. Case study in Central Italy

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Cited by 26 publications
(19 citation statements)
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“…Secondly, a slight increase begins from time order 5 that smoothly concludes in time order 13. This continuous and differentiated behavior (from 1 up to 13) may indicate a temporal dependence, persistent in the short and medium term, which is not detected by a correlogram (see Figure 4b, independent behavior in the intervals [3,4] and [10][11][12]). However, in a correlogam, there is also a lag (Time order) range where dependence raises between lags 5 and 9, as shown in Figure 4b, that noticeably coincides with a slight raise in dependence analysis though the BN approach (Figure 7b).…”
Section: Porma Rivermentioning
confidence: 88%
“…Secondly, a slight increase begins from time order 5 that smoothly concludes in time order 13. This continuous and differentiated behavior (from 1 up to 13) may indicate a temporal dependence, persistent in the short and medium term, which is not detected by a correlogram (see Figure 4b, independent behavior in the intervals [3,4] and [10][11][12]). However, in a correlogam, there is also a lag (Time order) range where dependence raises between lags 5 and 9, as shown in Figure 4b, that noticeably coincides with a slight raise in dependence analysis though the BN approach (Figure 7b).…”
Section: Porma Rivermentioning
confidence: 88%
“…SPI-Q regression model: SPI-Q [27,28] is a multi-linear regression model simulating the monthly inflow to surface reservoir through a calibrated linear combination of Standardized Precipitation Indices (SPI, [29]) computed for different cumulative time scales of the precipitation data gathered in the area. 2.…”
Section: Impact Modelmentioning
confidence: 99%
“…When spring flow measurements are not possible to carry out and there is not an appropriate knowledge about long time discharge series, spring discharge estimation is recommended. Many approaches have been proposed to analyze the relations between the rainfall time series over the recharge area and the spring outflow [5]. These models, for example, are based on continuous and discrete wavelet analysis [6,7], cross-correlation analysis [8,9,10], or machine learning models [11].…”
Section: Introductionmentioning
confidence: 99%
“…Afterwards, the model was applied to the Capodacqua di Spigno Spring, calibrating it on the available flow data, related to the years 1973-1977, as part of a scientific technical collaboration between the water agency Acqualatina S.p.A. and Sapienza University of Rome. The proposed model is compared to an existing and consolidated forecasting method that uses the SPI index for the estimation of the minimum annual spring discharge, a method already widely used in Italy and in many other countries [5,8]. The SPI analysis is often used internationally to study and characterize the hydrological drought [15,16,17,18].…”
Section: Introductionmentioning
confidence: 99%