An evaluation of ANN methods for estimating the lengths of hydraulic jumps in U-shaped channel Larbi Houichi, Noureddine Dechemi, Salim Heddam and Bachir Achour ABSTRACT Modelling of hydraulic characteristics of jump using theoretical and empirical models has always been a difcult task. The length of jump may be dened as the distance measured from the toe of the jump to the location of the surface rise. Due to high turbulence this length cannot be determined easily by theory. However, it has been investigated experimentally so as to design the stilling basins with hydraulic jumps. In this work, the control of a hydraulic jump by broad-crested sills in a U- shaped channel is recalled theoretically and experimentally examined. The study begins with a multiple regression (MR) analysis. Then, and in order to model the relative lengths of hydraulic jumps, we have implemented and evaluated two different articial neural networks (ANN): multilayer perceptron neural network (MLPNN) and generalized regression neural network (GRNN). The results demonstrate the predictive strength of GRNN and its potential to predict hydraulic problems with an adaptive spread value. However, the MLPNN model remains best classied by these indexes of performance. Larbi Houichi Research Laboratory in Applied Hydraulics, Department of hydraulics, University of Batna, Algeria Noureddine Dechemi Laboratory Construction and Environment, Polytechnical National School, Alger, Algeria Salim Heddam (corresponding author) Faculty of Science, Department of Agronomy, University of Skikda, Algeria E-mail: heddamsalim@yahoo.fr Bachir Achour Research Laboratory in Subterranean and Surface hydraulics, University of Biskra, Algeria Key words | articial neural network, GRNN, lengths of hydraulic jump, MLPNN, MR, U-channel NOMENCLATURE A Cross-sectional area of ow [m 2 ] D Diameter [m] Fr Froude number [] L j Length of jump [m] Q Discharge [m 3 /s] g Acceleration due to gravity [m/s 2 ] h Depth of ow [m] q Specic discharge [] y Relative depth of ow [] θ 1 Angle for semicircular cross-sectional area [rad] ABBREVIATIONS ANN Articial neural networks GRNN Generalized regression neural network MLPNN Multilayer perceptron neural network MR Multiple regression INTRODUCTION The hydraulic jump is the discontinuous transition between supercritical and subcritical ow with varied or xed location (Vischer & Hager ), it is characterized by a sudden increasing of the water surface with high turbulence production. This phenomenon is an example of steady non- uniform ow. Principally, the hydraulic jump is well known to hydraulic engineers as a useful means of dissipating excess energy of owing water downstream of hydraulic structures, such as spillways, chutes and sluices (Hager ). Some of the other practical applications are: e.g. ow-metering ume, mixing of chemicals for water puri- cation and aerating water (Chow ; Kucukali & Cokgor ). In practice, the stilling basin is seldom designed to conne the entire length of a free hydraulic jump on the paved apron, because such a basin would be too expensive. Consequently, accessories to control the jump are usually installed in the basin. The main purpose of such control is to shorten the range within which the jump will take place 147 © IWA Publishing 2013 Journal of Hydroinformatics | 15.1 | 2013 doi: 10.2166/hydro.2012.138