Artificial neural networks for estimation of temporal rate coefficient of equilibrium bar volume

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Özet

Present study consists the growth of a bar profile caused by cross-shore sediment transport. This is especially on growth of bar volume (V) toward equilibrium bar volume (Veq). Three analysis methods being a power and linear regression analysis (PRA and LRA) and an Artificial Neural Network (ANN) analysis were performed to determine empirical temporal rate coefficient (α). Forty-two experimental data were used for training set and the rest of the experimental data were used for testing set in the ANN analysis. As the results of analyses, the smallest average relative and root mean square error (RMSE) computed for the ANN methods are 7.578% and 0.029, respectively. It has been obtained that the ANN analysis, which is used for determination of α coefficient, gives reasonable results. Finally, bar volumes were calculated by means of computed α values and compared with the results of experimental data.

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dc.contributor.authorKankal, Murat
dc.contributor.authorKömürcü, Murat Ihsan
dc.contributor.authorYüksek, Ömer
dc.contributor.authorAkpinar, Adem
dc.date.accessioned2026-10-22T10:24:14.044039412Z
dc.date.available2026-10-22T10:24:14.044039412Z
dc.date.issued2012
dc.description.abstractPresent study consists the growth of a bar profile caused by cross-shore sediment transport. This is especially on growth of bar volume (V) toward equilibrium bar volume (Veq). Three analysis methods being a power and linear regression analysis (PRA and LRA) and an Artificial Neural Network (ANN) analysis were performed to determine empirical temporal rate coefficient (α). Forty-two experimental data were used for training set and the rest of the experimental data were used for testing set in the ANN analysis. As the results of analyses, the smallest average relative and root mean square error (RMSE) computed for the ANN methods are 7.578% and 0.029, respectively. It has been obtained that the ANN analysis, which is used for determination of α coefficient, gives reasonable results. Finally, bar volumes were calculated by means of computed α values and compared with the results of experimental data.
dc.identifier.eissn0975-1033
dc.identifier.endpage55
dc.identifier.issn2582-6506
dc.identifier.issue1
dc.identifier.scopus2-s2.0-84898917882
dc.identifier.startpage45
dc.identifier.urihttps://rdlopen.rawdatalibrary.net/r/gumushane/15593
dc.identifier.volume41
dc.identifier.wosWOS:000301614300006
dc.language.isoen
dc.publisherNational Institute of Science Communication and Policy Research
dc.relation.ispartofIndian Journal of Geo-Marine Sciences
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.subjectArtificial neural network
dc.subjectBar volume
dc.subjectCoastal profiles
dc.subjectSediment transport
dc.subjectTemporal variation
dc.subject.classificationOceanography
dc.subject.otherartificial neural network
dc.subject.otherbar
dc.subject.otherbeach profile
dc.subject.othercoastal zone
dc.subject.otherdata set
dc.subject.otherequilibrium
dc.subject.othererror analysis
dc.subject.otherregression analysis
dc.subject.othersediment transport
dc.subject.othertemporal variation
dc.titleArtificial neural networks for estimation of temporal rate coefficient of equilibrium bar volume
dc.typeArticle
rdl.citation.scopus3
rdl.citation.wos5
rdl.oa.statusclosed
rdl.scopus.quartileQ4
rdl.source.indexSCOPUS
rdl.source.indexWOS
rdl.wos.indexScience Citation Index Expanded (SCI-EXPANDED)