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Professor Advisordc.contributor.advisorOrtega Palma, Jaime
Professor Advisordc.contributor.advisorKadri, Usama
Authordc.contributor.authorMeza Valle, Claudio Alejandro 
Associate professordc.contributor.otherConca Rosende, Carlos
Associate professordc.contributor.otherFalcon Beas, Claudio
Associate professordc.contributor.otherLópez Ríos, Juan
Admission datedc.date.accessioned2019-10-09T19:15:30Z
Available datedc.date.available2019-10-09T19:15:30Z
Publication datedc.date.issued2019
Identifierdc.identifier.urihttps://repositorio.uchile.cl/handle/2250/171084
General notedc.descriptionTesis para optar al grado de Magíster en Ciencias de la Ingeniería, Mención Matemáticas Aplicadases_ES
Abstractdc.description.abstractExtreme waves generated in the ocean are of high importance because various maritime structures in the world, including ships, are confronted to this type of wave events, both in deep waters and in coastal areas. Some extreme waves correspond to wave phenomena generated in an atypical way in the ocean, also called monster waves, freak waves, rogue waves, extreme waves, solitons etc., since their generation differs from the common waves generated by wind. Assuming a slightly compressible ocean, the generation and analysis of acoustic-gravity waves (AGW or acoustic waves) in the ocean have been the subject of study for some time, because from them it is possible to obtain some information from the gravity wave, in this case a extreme wave that have generated them, and also to know other kind of phenomena induced by these AGW, as is the case of the bottom pressure. In the present work, a mathematical model has been developed which represents the generation and propagation of an extreme wave represented by a pressure change in the surface of the ocean considering compressible fluid, from which the generation and propagation of acoustic waves is induced. Since sound travels at a speed of 1500 m/s in the ocean, these waves arrive first at any observation point, allowing early detection of the extreme wave from the pressure in the oceanic bottom due to propagation of the acoustic wave. The theoretical development and two-dimensional numerical simulations are presented in the document. The implementation of this methodology and its results is relevant in the field of civil and maritime engineering in Chile since its high potential in coastal zones, due to the fact that for some years, the frequency of extreme wave events has been seen increased, and having an alternative detection system for extreme wave events can become a relevant factor in coastal management and natural disasters services. It is important to mention that this type of work has not been developed previously in Chile.es_ES
Patrocinadordc.description.sponsorshipproyectos Centros de Excelencia Basal Conicyt PIA AFB 170001 CMM & UMI-CNRS 2807 y Fondecyt Regular 1171854es_ES
Lenguagedc.language.isoenes_ES
Publisherdc.publisherUniversidad de Chilees_ES
Type of licensedc.rightsAttribution-NonCommercial-NoDerivs 3.0 Chile*
Link to Licensedc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/*
Keywordsdc.subjectOlases_ES
Keywordsdc.subjectOndas de agua - Modelos matemáticoses_ES
Keywordsdc.subjectONDAS SONORAS - Modelos matemáticoses_ES
Títulodc.titleEarly detection of extreme waves by acoustic gravity-waveses_ES
Document typedc.typeTesis
Catalogueruchile.catalogadorgmmes_ES
Departmentuchile.departamentoDepartamento de Ingeniería Matemáticaes_ES
Facultyuchile.facultadFacultad de Ciencias Físicas y Matemáticases_ES


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Attribution-NonCommercial-NoDerivs 3.0 Chile
Except where otherwise noted, this item's license is described as Attribution-NonCommercial-NoDerivs 3.0 Chile