dc.contributorUniversidade Estadual Paulista (Unesp)
dc.contributorRio de Janeiro Federal University
dc.date.accessioned2014-05-27T11:20:34Z
dc.date.accessioned2022-10-05T17:48:03Z
dc.date.available2014-05-27T11:20:34Z
dc.date.available2022-10-05T17:48:03Z
dc.date.created2014-05-27T11:20:34Z
dc.date.issued2002-12-01
dc.identifierProceedings of the Third International Conference on Engineering Computational Technology, p. 99-100.
dc.identifierhttp://hdl.handle.net/11449/67100
dc.identifier10.4203/ccp.76.38
dc.identifier2-s2.0-0036931618
dc.identifier5808118510418914
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/3916786
dc.description.abstractWater waves generated by landslides were long menace in certain localities and the study of this phenomenon were carried out at an accelerated rate in the last decades. Nevertheless, the phase of wave creation was found to be very complex. As such, a numerical model based on Boussinesq equations was used to describe water waves generated by local disturbance. This numerical model takes in account the vertical acceleration of the particles and considers higher orders derivate terms previously neglected by Boussinesq, so that in the generation zone, this model can support high relative amplitude of waves.
dc.languageeng
dc.relationProceedings of the Third International Conference on Engineering Computational Technology
dc.rightsAcesso aberto
dc.sourceScopus
dc.subjectBoussinesq equations
dc.subjectExperimental analysis
dc.subjectLandslides
dc.subjectLong waves
dc.subjectNumerical simulations
dc.subjectSerres equations
dc.subjectComputer simulation
dc.subjectFriction
dc.subjectMathematical models
dc.subjectShock waves
dc.subjectWater waves
dc.titleWater waves generated by local disturbance: Serre's model validity
dc.typeTrabalho apresentado em evento


Este ítem pertenece a la siguiente institución