2015
DOI: 10.3808/jei.201500309
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Application of Entropy Concept for Input Selection of Wavelet-ANN based Rainfall-Runoff Modeling

Abstract: This paper presents a Wavelet-based Artificial Neural Network (WANN) approach to model rainfall-runoff process of the Delaney Creek and Payne Creek watersheds with distinct hydro-geomorphological characteristics, located in Florida. Wavelet is utilized to handle the multi-frequency characteristics of the process in daily and monthly time scales. Thus, rainfall and runoff time series were decomposed into several sub-series by various mother wavelets. Due to multiple components obtained through wavelet decomposi… Show more

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Cited by 25 publications
(21 citation statements)
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“…Because of the existence of temporal heterogeneity in hydrological systems, the calibration efficiency may not be very high. Data uncertainties as well as other types of uncertainties may lead to instability of the DPMI modelling efficiencies (Ahmadi et al ., ; Nourani et al ., ; Rahmani and Zarghami, ; Shen et al ., ; Wang et al ., ). Simplifications in the process of DPMI , such as quantification of the correspondence between predictors and streamflow as the principal monotonicity, may also decrease the capability of DPMI at reflecting real‐world hydrological systems.…”
Section: Discussionmentioning
confidence: 99%
“…Because of the existence of temporal heterogeneity in hydrological systems, the calibration efficiency may not be very high. Data uncertainties as well as other types of uncertainties may lead to instability of the DPMI modelling efficiencies (Ahmadi et al ., ; Nourani et al ., ; Rahmani and Zarghami, ; Shen et al ., ; Wang et al ., ). Simplifications in the process of DPMI , such as quantification of the correspondence between predictors and streamflow as the principal monotonicity, may also decrease the capability of DPMI at reflecting real‐world hydrological systems.…”
Section: Discussionmentioning
confidence: 99%
“…In DPMI, the responsive relationship from influencing factors (named as predictors) to the hydrological variable of interest (named as the predictand) will be discretized as interrelated end nodes, i.e. groups of paired samples of predictors and the predictand, under irregular nonlinearities, data uncertainties, and multivariate dependencies (Ahmadi et al ., ; Nourani et al ., ; Rahmani and Zarghami, ; Shen et al ., ; Wang et al ., ). In detail, a discrete distribution transformation approach will be developed to enable transformation of non‐normally distributed predictand samples as a normal distribution and invertible restoration of the simulated predictand values as the original non‐normal distribution.…”
Section: Introductionmentioning
confidence: 99%
“…In addition, a simpler model structure means that the propagation of uncertainty from different sources is easier to assess. The use of data-driven models, such as neural networks, statistical methods or regression-based techniques (e.g., Li et al, 2015b, Li et al, 2015cYang et al, 2015), has been widespread in hydrology, particularly for short term daily flow rate forecasts, using a variety of input variables (Garen, 1992;Zealand et al, 1999;Campolo et al, 1999;Schilling and Walter, 2005;Adamowski and Sun, 2010;Duncan et al, 2011;Li et al, 2015a;Nourani et al, 2015). A recent regression based study predicted flow in the Bow River in Calgary, using a base difference regression model (Veiga et al, 2014).…”
Section: Introductionmentioning
confidence: 99%