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dc.creatorEscalante Sánchez, Ciprianoes
dc.creatorFernández Nieto, Enrique Domingoes
dc.creatorGarres-Díaz, Josées
dc.creatorMorales de Luna, Tomáses
dc.creatorPenel, Yohanes
dc.date.accessioned2023-11-29T07:42:00Z
dc.date.available2023-11-29T07:42:00Z
dc.date.issued2023-05-10
dc.identifier.citationEscalante Sánchez, C., Fernández Nieto, E.D., Garres-Díaz, J., Morales de Luna, T. y Penel, Y. (2023). Non-hydrostatic layer-averaged approximation of Euler system with enhanced dispersion properties. Computational and Applied Mathematics, 42 (177). https://doi.org/10.1007/s40314-023-02309-7.
dc.identifier.issn0101-8205es
dc.identifier.issn1807-0302es
dc.identifier.urihttps://hdl.handle.net/11441/151791
dc.description.abstractA new family of non-hydrostatic layer-averaged models for the non-stationary Euler equations is presented in this work, with improved dispersion relations. They are a generalisation of the layer-averaged models introduced in Fernández-Nieto et al. (Commun Math Sci 16(05):1169–1202, 2018), named LDNH models, where the vertical profile of the horizontal velocity is layerwise constant. This assumption implies that solutions of LDNH can be seen as a first order Galerkin approximation of Euler system. Nevertheless, it is not a fully (x, z) Galerkin discretisation of Euler system, but just in the vertical direction (z). Thus, the resulting model only depends on the horizontal space variable (x), and therefore specific and efficient numerical methods can be applied (see Escalante-Sanchez et al. in J Sci Comput 89(55):1–35, 2021). This work focuses on particular weak solutions where the horizontal velocity is layerwise linear on z and possibly discontinuous across layer interfaces. This approach allows the system to be a second-order approximation in the vertical direction of Euler system. Several closure relations of the layer-averaged system with non-hydrostatic pressure are presented. The resulting models are named LIN-NHk models, with k = 0, 1, 2. Parameter k indicates the degree of the vertical velocity profile considered in the approximation of the vertical momentum equation. All the introduced models satisfy a dissipative energy balance. Finally, an analysis and a comparison of the dispersive properties of each model are carried out. We show that Models LIN-NH and LIN-NH provide a better dispersion relation, group velocity and shoaling than LDNH models.es
dc.formatapplication/pdfes
dc.format.extent38 p.es
dc.language.isoenges
dc.publisherSpringeres
dc.relation.ispartofComputational and Applied Mathematics, 42 (177).
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internacional*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.subjectNon-hydrostatic layer-averaged modelses
dc.subjectNon-stationary Euler equationses
dc.subjectGalerkin approximationes
dc.titleNon-hydrostatic layer-averaged approximation of Euler system with enhanced dispersion propertieses
dc.typeinfo:eu-repo/semantics/articlees
dcterms.identifierhttps://ror.org/03yxnpp24
dc.type.versioninfo:eu-repo/semantics/publishedVersiones
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses
dc.contributor.affiliationUniversidad de Sevilla. Departamento de Matemática Aplicada I (ETSII)es
dc.contributor.affiliationUniversidad de Sevilla. Departamento de Matemática Aplicada II (ETSI)es
dc.relation.projectIDRTI2018-096064-B-C2(1/2)es
dc.relation.projectIDPID2020-114688RB-I00es
dc.relation.publisherversionhttps://link.springer.com/article/10.1007/s40314-023-02309-7es
dc.identifier.doi10.1007/s40314-023-02309-7es
dc.contributor.groupUniversidad de Sevilla. FQM120: Modelado Matemático y Simulación de Sistemas Medioambientaleses
dc.journaltitleComputational and Applied Mathematicses
dc.publication.volumen42es
dc.publication.issue177es
dc.contributor.funderGobierno de Españaes
dc.contributor.funderEuropean Commission (EC). Fondo Europeo de Desarrollo Regional (FEDER)es

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