Abstract
In this study, a network using radial basis functions as the mapping function in the evolutionary equation for prediction of time series is presented. A radial basis function network requires the determination of the number of centres of the radial basis functions, their receptive field widths, and the linear weights of the network output layer. Methods to estimate the widths of the receptive fields, and the number of centres for the radial basis functions are introduced in the study. The latter is based on the concept of the Generalized Degrees of Freedom. The linear weights are determined by the least squares method. The predictions by the proposed method when compared with the actual values of four hydrometeorological data sets, are better than those by the traditional approach of fixing the number of centres. Copyright © 2003 International Association of Hydrological Sciences.
Original language | English |
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Title of host publication | Water resources systems: Water availability and global change |
Editors | Stewart FRANKS, Gunter BLOSCHL, Michio KUMAGAI, Katumi MUSIAKE, Dan ROSBJERG |
Place of Publication | Wallingford, Oxfordshire |
Publisher | International Association of Hydrological Sciences |
Pages | 260-266 |
ISBN (Print) | 9781901502279 |
Publication status | Published - 2003 |
Citation
Jayawardena, A. W., Xu, P., & Li, W. K. (2003). Radial basis function network for prediction of hydrological time series. In S. Franks, G. Bloschl, M. Kumagai, K. Musiake, & D. Rosbjerg (Eds.), Water resources systems: Water availability and global change (pp. 260-266). Wallingford, Oxfordshire: International Association of Hydrological Sciences.Keywords
- Chao Phraya River, chaos
- Generalized degrees of freedom
- Mekong River
- Phase space
- Radial basis functions
- S-index