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Cited by 547

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Using support vector machines for long-term discharge prediction

Open access
LIN, JIAN-YI, CHENG, CHUN-TIAN, CHAU, KWOK-WING·2006·Hydrological Sciences Journal

Abstract

Accurate time- and site-specific forecasts of streamflow and reservoir inflow are important in effective hydropower reservoir management and scheduling. Traditionally, autoregressive moving-average (ARMA) models have been used in modelling water resource time series as a standard representation of stochastic time series. Recently, artificial neural network (ANN) approaches have been proven to be efficient when applied to hydrological prediction. In this paper, the support vector machine (SVM) is presented as a promising method for hydrological prediction. Over-fitting and local optimal solution are unlikely to occur with SVM, which implements the structural risk minimization principle rather than the empirical risk minimization principle. In order to identify appropriate parameters of the SVM prediction model, a shuffled complex evolution algorithm is performed through exponential transformation. The SVM prediction model is tested using the long-term observations of discharges of monthly river flow discharges in the Manwan Hydropower Scheme. Through the comparison of its performance with those of the ARMA and ANN models, it is demonstrated that SVM is a very potential candidate for the prediction of long-term discharges.

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Metadata

Authors
LIN, J.-Y., CHENG, C.-T., & CHAU, K.-W.
Venue
Hydrological Sciences Journal
Published
2006-08
Volume
51
Issue
4
Pages
599-612
ISSN
  • 0262-6667 (ISSN-L)
  • 2150-3435
OpenAlex
W2057018326
Cited by
547
References
1
FWCI
9.12
Type
journal article
Language
en
Open access
bronze

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CoChat. (2026). Citation check: Using support vector machines for long-term discharge prediction. https://app.cochat.ai/papers/10.1623/hysj.51.4.599
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LIN, J.-Y., CHENG, C.-T., & CHAU, K.-W. (2006). Using support vector machines for long-term discharge prediction. Hydrological Sciences Journal. https://doi.org/10.1623/hysj.51.4.599

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