dc.contributor | Universidade Estadual Paulista (Unesp) | |
dc.contributor | Rio de Janeiro Federal University | |
dc.date.accessioned | 2014-05-27T11:20:34Z | |
dc.date.accessioned | 2022-10-05T17:48:03Z | |
dc.date.available | 2014-05-27T11:20:34Z | |
dc.date.available | 2022-10-05T17:48:03Z | |
dc.date.created | 2014-05-27T11:20:34Z | |
dc.date.issued | 2002-12-01 | |
dc.identifier | Proceedings of the Third International Conference on Engineering Computational Technology, p. 99-100. | |
dc.identifier | http://hdl.handle.net/11449/67100 | |
dc.identifier | 10.4203/ccp.76.38 | |
dc.identifier | 2-s2.0-0036931618 | |
dc.identifier | 5808118510418914 | |
dc.identifier.uri | http://repositorioslatinoamericanos.uchile.cl/handle/2250/3916786 | |
dc.description.abstract | Water 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.language | eng | |
dc.relation | Proceedings of the Third International Conference on Engineering Computational Technology | |
dc.rights | Acesso aberto | |
dc.source | Scopus | |
dc.subject | Boussinesq equations | |
dc.subject | Experimental analysis | |
dc.subject | Landslides | |
dc.subject | Long waves | |
dc.subject | Numerical simulations | |
dc.subject | Serres equations | |
dc.subject | Computer simulation | |
dc.subject | Friction | |
dc.subject | Mathematical models | |
dc.subject | Shock waves | |
dc.subject | Water waves | |
dc.title | Water waves generated by local disturbance: Serre's model validity | |
dc.type | Trabalho apresentado em evento | |