{"id":10267,"date":"1996-01-01T00:00:00","date_gmt":"1996-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/1996\/01\/01\/interaccion-no-lineal-entre-los-flujos-subinerciales-y-mareales-asociados-al-regimen-barotropico-en-el-estrecho-de-gibraltar\/"},"modified":"1996-01-01T00:00:00","modified_gmt":"1996-01-01T00:00:00","slug":"interaccion-no-lineal-entre-los-flujos-subinerciales-y-mareales-asociados-al-regimen-barotropico-en-el-estrecho-de-gibraltar","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/interaccion-no-lineal-entre-los-flujos-subinerciales-y-mareales-asociados-al-regimen-barotropico-en-el-estrecho-de-gibraltar\/","title":{"rendered":"Interaccion no lineal entre los flujos subinerciales y mareales asociados al regimen barotropico en el estrecho de gibraltar."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Rafael Ma\u00f1anes Salinas <\/strong><\/h2>\n<p>En la presente memoria se profundiza en el conocimiento del fenomeno de interaccion no lineal entre las frecuencias astronomicas de la banda semidiurna con las frecuencias bajas o subinerciales en el entorno definido por el estrecho de gibraltar.Se pone de manifiesto mediante el uso de diferentes tecnicas de tratamiento de se\u00f1ales &#8211; analisis armonico, analisis espectral cruzado, filtros, descomposicion en funciones empiricas ortogonales -, la existencia de distorsiones en la amplitud y fase de la se\u00f1al de la onda m2 (elegida como representativa de la banda semidiurna en el estrecho) y como contribuyen de manera diferenciada a la serie residual las distorsiones en amplitud y en fase.En los siguientes capitulos se propone a la interaccion no lineal entre la se\u00f1al de m2 y las frecuencias subinerciales como la responsable de esas distorsiones.  para comprobar esta hipotesis se formula un modelo cuasi-analitico de segundo orden, que caracteriza a este tipo de interaccion. Se obtiene la solucion particularizada para el estrecho de gibraltar y por ultimo se procede a validar los resultados experimentales obtenidos con el modelo, con los resultados experimentales. Observandose un alto grado de correlacion entre las series teoricas y las experimentales.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Interaccion no lineal entre los flujos subinerciales y mareales asociados al regimen barotropico en el estrecho de gibraltar.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Interaccion no lineal entre los flujos subinerciales y mareales asociados al regimen barotropico en el estrecho de gibraltar. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Rafael Ma\u00f1anes Salinas <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 C\u00e1diz<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1996<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n<h3>Direcci\u00f3n y tribunal<\/h3>\n<ul>\n<li><strong>Director de la tesis<\/strong>\n<ul>\n<li>Luis Tomas Tejedor Martinez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Francisco Lopez  Aguayo <\/li>\n<li>Jes\u00fas Garcia Lafuente (vocal)<\/li>\n<li>Ra\u00fal Medina Santamar\u00eda (vocal)<\/li>\n<li>Sebastian Monserrat Antich (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Rafael Ma\u00f1anes Salinas En la presente memoria se profundiza en el conocimiento del fenomeno de interaccion no [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center 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