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dc.contributor.authorAntuono, M
dc.contributor.authorValenza, S
dc.contributor.authorLugni, Claudio
dc.contributor.authorColicchio, Giuseppina
dc.date.accessioned2019-12-19T07:30:46Z
dc.date.available2019-12-19T07:30:46Z
dc.date.created2019-08-26T12:40:30Z
dc.date.issued2019
dc.identifier.citationPhysics of Fluids. 2019, 31 (2), 1-17.nb_NO
dc.identifier.issn1070-6631
dc.identifier.urihttp://hdl.handle.net/11250/2634064
dc.description.abstractThe present work completes the validation of the depth-semi-averaged model defined in Antuono et al. [“A depth semi-averaged model for coastal dynamics,” Phys. Fluids 29, 056603 (2017)] providing a numerical implementation in three spatial dimensions. In particular, the model is aimed at describing a wide variety of phenomena typical of the coastal region, as for example nonlinear interaction between waves and the bottom bathymetry (diffraction/refraction phenomena), dispersion effects, and beach inundation. To this purpose, the proposed scheme is tested against benchmark experimental data available in the literature for wave propagation problems in both intermediate and shallow water conditions. A final simulation is carried out by considering a tsunami wave running over a prototype bathymetry resembling a bay-promontory coastline. Different widths of the bay have been considered, describing their influence on the run-up dynamics.nb_NO
dc.language.isoengnb_NO
dc.publisherAIP Publishing, American Institute of Physicsnb_NO
dc.titleValidation of a three-dimensional depth-semi-averaged modelnb_NO
dc.typeJournal articlenb_NO
dc.typePeer reviewednb_NO
dc.description.versionacceptedVersionnb_NO
dc.source.pagenumber1-17nb_NO
dc.source.volume31nb_NO
dc.source.journalPhysics of Fluidsnb_NO
dc.source.issue2nb_NO
dc.identifier.doi10.1063/1.5080307
dc.identifier.cristin1718698
dc.description.localcodeThis is the authors’ accepted and refereed manuscript to the article. This article may be downloaded for personal use only. Any other use requires prior permission of the author and AIP Publishing. The following article appeared in Physics of Fluids 31, 026601 (2019) and may be found at https://doi.org/10.1063/1.5080307.nb_NO
cristin.unitcode194,64,20,0
cristin.unitnameInstitutt for marin teknikk
cristin.ispublishedtrue
cristin.fulltextpostprint
cristin.qualitycode2


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