Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/99565
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dc.contributorDepartment of Civil and Environmental Engineering-
dc.creatorXu, DMen_US
dc.creatorWang, Xen_US
dc.creatorWang, WCen_US
dc.creatorChau, KWen_US
dc.creatorZang, HFen_US
dc.date.accessioned2023-07-14T02:49:35Z-
dc.date.available2023-07-14T02:49:35Z-
dc.identifier.issn1464-7141en_US
dc.identifier.urihttp://hdl.handle.net/10397/99565-
dc.language.isoenen_US
dc.publisherInternational Water Association Publishingen_US
dc.rights© 2023 The Authorsen_US
dc.rightsThis is an Open Access article distributed under the terms of the Creative Commons Attribution Licence (CC BY 4.0), which permits copying, adaptation and redistribution, provided the original work is properly cited (http://creativecommons.org/licenses/by/4.0/).en_US
dc.rightsThe following publication Xu, D. M., Wang, X., Wang, W. C., Chau, K. W., & Zang, H. F. (2023). Improved monthly runoff time series prediction using the SOA–SVM model based on ICEEMDAN–WD decomposition. Journal of Hydroinformatics, 25(3), 943-970 is available at https://doi.org/10.2166/hydro.2023.172.en_US
dc.subjectImproved complete ensemble EMD (ICEEMDAN)en_US
dc.subjectMonthly runoff predictionen_US
dc.subjectQuadratic decompositionen_US
dc.subjectSeagull optimization algorithm (SOA)en_US
dc.subjectSupport vector machine (SVM)en_US
dc.subjectWavelet decomposition (WD)en_US
dc.titleImproved monthly runoff time series prediction using the SOA–SVM model based on ICEEMDAN–WD decompositionen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.spage943en_US
dc.identifier.epage970en_US
dc.identifier.volume25en_US
dc.identifier.issue3en_US
dc.identifier.doi10.2166/hydro.2023.172en_US
dcterms.abstractIn runoff prediction, the prediction accuracy is often affected by the non-linear and non-stationary characteristics of the runoff series. In this study, a coupled forecasting model is proposed that decomposes the original runoff series by an improved complete ensemble Empirical Mode Decomposition (EMD) (ICEEMDAN) combined with a wavelet decomposition (WD) and then forecasts the monthly runoff using a support vector machine (SVM) optimized by the seagull optimization algorithm (SOA). In this method, a series of Intrinsic Mode Function (IMF) and a Residual (Res) are obtained by decomposing the original runoff series with ICEEMDAN. The WD method is used to perform quadratic decomposition of high-frequency components decomposed by the ICEEMDAN method to make the runoff series as smooth as possible. Then the decomposed components are input into the SOA-SVM model for prediction. Finally, the prediction results of each component are superimposed and reconstructed to obtain the final monthly runoff prediction results. RMSE, Mean Absolute Percentage Error (MAPE), Nash-Sutcliffe Efficiency Coefficient (NSEC), and R are selected to evaluate the prediction results and the model is compared with SOA-SVM model, EMD-SOA-SVM model and CEEMDAN-SOA-SVM model other models. The proposed model is applied to the monthly runoff forecast of the Hongjiadu and Manwan Reservoirs. When compared with other benchmarking models, the ICEEMDAN-WD-SOA-SVM model attains the smallest Root Mean Square Error (RMSE) and MAPE and the largest NSEC and R. The ICEEMDAN-WD-SOA-SVM model has the best prediction effect, the highest prediction accuracy, and the lowest prediction error.-
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationJournal of hydroinformatics, 1 May. 2023, v. 25, no. 3, p. 943-970en_US
dcterms.isPartOfJournal of hydroinformaticsen_US
dcterms.issued2023-05-01-
dc.description.validate202307 bckw-
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_Others-
dc.description.fundingSourceOthersen_US
dc.description.fundingTextSpecial project for collaborative innovation of science and technology in 2021; Henan Province University Scientific and Technological Innovation Teamen_US
dc.description.pubStatusPublisheden_US
dc.description.TAIWAP (2023) -“Subscribe to Open” since 2021en_US
dc.description.oaCategoryTAen_US
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