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A combined model for tsunami wave propagation, dispersion, breaking and fluid-structure interaction

datacite.subject.fosCiências Naturais::Ciências da Terra e do Ambientept_PT
dc.contributor.advisorBaptista, Maria Ana de Carvalho Viana
dc.contributor.advisorValente, Paulo Alexandre de Avilez Rodrigues de Almeida
dc.contributor.advisorMiranda, Jorge Miguel Alberto de
dc.contributor.authorLima, Vânia
dc.date.accessioned2023-01-03T16:36:45Z
dc.date.available2023-01-03T16:36:45Z
dc.date.issued2022-04
dc.date.submitted2020-07
dc.description.abstractIn this work, a fully combined tsunami model was developed, by coupling a sequence of 3 distinct numerical models, with different characteristics, for particular phases of the tsunami lifecycle. The computational codes that compose the fully combined tsunami model are the GeoClaw code, the FUNWAVE-TVD code and the OpenFOAM code, via the olaFlow solver. The coupling of GeoClaw with FUNWAVE-TVD was designated as the combined model 1 (CM1) and the combination of FUNWAVE-TVD/CM1 with the CFD code was designated as the combined model 2 (CM2). The full combination of both CM1 and CM2 resulted in the fully combined tsunami model CM. To achieve the coupling between numerical models, individual coupling methodologies were approached, tested and analysed. For the CM1, we choose a refined covered gauge domain coupling methodology and for the CM2 a timeSeries condition coupling methodology was used, which applied waveType wavemaker and the waveTheory tveta, from the olaFlow module. The validation of the individual numerical codes and of the combined model patches was performed with both numerical and physical test cases. Several physical experiments were carried out to generate both solitary and N-waves and a novel first-order theoretical formulation, necessary to generate N-waves experimentally, by means of a piston wave generating system, was developed and detailed in this work. The large-scale physical experiments were performed in the wave basin and in a beach composed by a 1:15 plane slope and a 1:30 plane slope. The generated solitary and N-waves were classified according to their Stokes number. Experimental free surface elevation, run-in, run-up and pressure measurements were retrieved from the physical experiments. Run-in, run-up and pressure laws were proposed for solitary waves and N-waves respectively. The experimental measurements were compared with numerical simulation results. The objectives of the development of the fully combined tsunami model were (1) to join the advantages of the individual models in a single one, attempting to increase the accuracy, efficiency and regime of validity, and (2) to bring a contribution in the tackling of some of the existing problems and challenges of tsunami science, such as the frequency dispersion in long distance tsunami propagation, the complex tsunami on land propagation and fluid flow interactions with river courses and with the coastal and urban areas. The fully combined tsunami model CM simulation results for a Mω 8.5 Earthquake and Tsunami hitting the Portuguese coast showed the ability of the combined model to cover all the tsunami stages. We show that with a 2DV simulation of the CFD code for the Marina of Cascais bathymetric and topographic profile it was possible to observe the vortices behind the breakwater. The analysis of the free surface elevation, velocities and pressure of the tsunami waves was performed. This allowed us to understand the consequence of three diferent tsunami waves scenarios after the breakwater zone. It was possible to draw some brief conclusions considering the tsunami impact. The fully combined tsunami model achieved in this work is a novelty, since it is composed by a sequence of distinct numerical models, including the three-dimensional component granted by the CFD code. With this combined model, it is possible to perform the simulation of real case tsunami events and hypothetical scenarios, applying real or synthetic tsunami-type wave profiles, studying and researching the impact and the tsunami interaction with the coastal areas.pt_PT
dc.identifier.tid101495773pt_PT
dc.identifier.urihttp://hdl.handle.net/10451/55610
dc.language.isoengpt_PT
dc.relationNORTE-01-0145-FEDER-000035pt_PT
dc.relationA Combined Model for Tsunami Wave Propagation, Dispersion, Breaking and Fluid-Structure Interaction
dc.subjectmodelo de tsunami totalmente combinadopt_PT
dc.subjectondas solitárias e ondas Npt_PT
dc.subjectGeoClawpt_PT
dc.subjectFUNWAVE-TVDpt_PT
dc.subjectOpenFOAM – olaFlowpt_PT
dc.subjectfully combined tsunami modelpt_PT
dc.subjectsolitary and N-wavespt_PT
dc.titleA combined model for tsunami wave propagation, dispersion, breaking and fluid-structure interactionpt_PT
dc.typedoctoral thesis
dspace.entity.typePublication
oaire.awardNumberSFRH/BD/96725/2013
oaire.awardTitleA Combined Model for Tsunami Wave Propagation, Dispersion, Breaking and Fluid-Structure Interaction
oaire.awardURIinfo:eu-repo/grantAgreement/FCT//SFRH%2FBD%2F96725%2F2013/PT
person.familyNameVeloso de Azevedo Lima
person.givenNameVânia Cristina
person.identifierH-2558-2019
person.identifier.ciencia-id411C-292C-8688
person.identifier.orcid0000-0003-2653-2649
person.identifier.scopus-author-id55360847600
project.funder.identifierhttp://doi.org/10.13039/501100001871
project.funder.nameFundação para a Ciência e a Tecnologia
rcaap.rightsopenAccesspt_PT
rcaap.typedoctoralThesispt_PT
relation.isAuthorOfPublication88f86ef3-6345-467e-a404-69d9e6c6e4d0
relation.isAuthorOfPublication.latestForDiscovery88f86ef3-6345-467e-a404-69d9e6c6e4d0
relation.isProjectOfPublication47afcb52-99b7-4776-b185-22012a8c9c3e
relation.isProjectOfPublication.latestForDiscovery47afcb52-99b7-4776-b185-22012a8c9c3e
thesis.degree.nameTese de doutoramento, Ciências Geofísicas e da Geoinformação (Geofísica), Universidade de Lisboa, Faculdade de Ciências, 2022pt_PT

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