Galerkin's formulation of the finite elements method to obtain the depth of closure

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Campo DCValorIdioma
dc.contributorIngeniería del Terreno y sus Estructuras (InTerEs)es_ES
dc.contributorIngeniería del Transporte, Territorio y Medio Litoral (AORTA)es_ES
dc.contributorModelización Matemática de Sistemases_ES
dc.contributor.authorAragonés, Luis-
dc.contributor.authorPagán, José Ignacio-
dc.contributor.authorLópez, Isabel-
dc.contributor.authorNavarro-González, Francisco J.-
dc.contributor.authorVillacampa, Yolanda-
dc.contributor.otherUniversidad de Alicante. Departamento de Ingeniería Civiles_ES
dc.contributor.otherUniversidad de Alicante. Departamento de Matemática Aplicadaes_ES
dc.date.accessioned2019-02-21T14:18:13Z-
dc.date.available2019-02-21T14:18:13Z-
dc.date.issued2019-04-10-
dc.identifier.citationScience of The Total Environment. 2019, 660: 1256-1263. doi:10.1016/j.scitotenv.2019.01.017es_ES
dc.identifier.issn0048-9697 (Print)-
dc.identifier.issn1879-1026 (Online)-
dc.identifier.urihttp://hdl.handle.net/10045/88558-
dc.description.abstractCoastal erosion and lack of sediment supply are a serious global problem. It is therefore necessary to determine the depth of closure (DoC) of a beach—key parameter in the calculation of the sand volume and the location of the beach protection elements—in a precise way. For this reason, this work generates a numerical model based on Galerkin's formulation of finite elements that provides sufficient precision for the determination of DoC with a minimum investment. Thus, after the generation of three models in which the difference was the dependent variables, the least complex has been chosen. It is composed of the variables: median sediment size, wave height and period associated with the mean flow, as well as the angle that the mean flow forms with respect to the studied profile in absolute value (α). The selected model has been compared with the most commonly used models currently in use, having an average absolute error of 0.36 m and an average MAPE of <7.5%, which represents an improvement of >70% over current models. In addition, it presents a high stability, since after the random disturbance of all the input variables (up to 5%), the model error remains stable, increasing the MAPE by a maximum of 7.4% and the average absolute error by 0.15 m. Therefore, it is possible to use the model to infer the DoC in other study areas where the values of the variables are similar to those studied here, although the selected method can be extrapolated to other parts of the world.es_ES
dc.description.sponsorshipThis work was partially supported by the Universidad de Alicante through the project “Estudio sobre el perfil de equilibrio y la profundidad de cierre en playas de arena” (GRE15-02).es_ES
dc.languageenges_ES
dc.publisherElsevieres_ES
dc.rights© 2019 Elsevier B.V.es_ES
dc.subjectDepth of closurees_ES
dc.subjectSedimentes_ES
dc.subjectGalerkines_ES
dc.subjectNumerical modeles_ES
dc.subjectPosidonia oceanicaes_ES
dc.subject.otherIngeniería e Infraestructura de los Transporteses_ES
dc.subject.otherMatemática Aplicadaes_ES
dc.titleGalerkin's formulation of the finite elements method to obtain the depth of closurees_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.peerreviewedsies_ES
dc.identifier.doi10.1016/j.scitotenv.2019.01.017-
dc.relation.publisherversionhttps://doi.org/10.1016/j.scitotenv.2019.01.017es_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
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