Modeling of streamflow- suspended sediment load relationship by adaptive neuro-fuzzy and artificial neural network approaches (Case study: Dalaki River, Iran)
نویسندگان
1 PhD Student, Faculty of Natural Resources, University of Tehran, Karaj, I.R. Iran
2 Associate Professor, Faculty of Natural Resources, University of Tehran, Tehran, Iran
3 MSc. Graduate, International Desert Research Center, University of Tehran, Tehran, Iran
doi
10.22059/jdesert.2015.56481چکیده
Modeling of stream flow–suspended sediment relationship is one of the most studied topics in hydrology due to itsessential application to water resources management. Recently, artificial intelligence has gained much popularity owing toits application in calibrating the nonlinear relationships inherent in the stream flow–suspended sediment relationship. Thisstudy made us of adaptive neuro-fuzzy inference system (ANFIS) techniques and three artificial neural networkapproaches, namely, the Feed-forward back-propagation (FFBP), radial basis function-based neural networks (RBF),geomorphology-based artificial neural network (GANN) to predict the streamflow suspended sediment relationship. Toillustrate their applicability and efficiency,, the daily streamflow and suspended sediment data of Dalaki River station insouth of Iran were used as a case study. The obtained results were compared with the sediment rating curve (SRC) andregression model (RM). Statistic measures (RMSE, MAE, and R2) were used to evaluate the performance of the models.From the results, adaptive neuro-fuzzy (ANFIS) approach combined capabilities of both Artificial Neural Networks andFuzzy Logic and then reflected more accurate predictions of the system. The results showed that accuracy of estimationsprovided by ANFIS was higher than ANN approaches, regression model and sediment rating curve. Additionally, relatingselected geomorphologic parameters as the inputs of the ANN with rainfall depth and peak runoff rate enhanced theaccuracy of runoff rate, while sediment loss predictions from the watershed and GANN model performed better than theother ANN approaches together witj regression equations in Modeling of stream flow–suspended sediment relationship.