{"id":37256,"date":"1998-01-01T00:00:00","date_gmt":"1998-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/simulacion-numerica-de-procesos-oceanograficos-en-las-costas-atlanticas-espanolas\/"},"modified":"1998-01-01T00:00:00","modified_gmt":"1998-01-01T00:00:00","slug":"simulacion-numerica-de-procesos-oceanograficos-en-las-costas-atlanticas-espanolas","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/simulacion-numerica-de-procesos-oceanograficos-en-las-costas-atlanticas-espanolas\/","title":{"rendered":"Simulacion numerica de procesos oceanograficos en las costas atlanticas espa\u00f1olas."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Enrique \u00e1lvarez Fanjul <\/strong><\/h2>\n<p>El objetivo de esta tesis es estudiar, en las aguas atl\u00e1nticas espa\u00f1olas, la circulaci\u00f3n mesoscalar inducida por el viento, las mareas y los gradientes barocl\u00ednicos.  la principal herramienta empleada en este trabajo es el modelo de circulaci\u00f3n oce\u00e1nica hamsom. Los fen\u00f3menos estudiados se presentan divididos en funci\u00f3n de la velocidad de su variabilidad temporal. En primer lugar se estudian los de tipo clim\u00e1tico (circulaci\u00f3n media inducida por viento, gradientes barocl\u00ednicos, etc&#8230;) para proseguir por el an\u00e1lisis de los procesos de r\u00e1pida variabilidad (mareas y ondas de tormenta). El \u00faltimo cap\u00edtulo est\u00e1 dedicado a explorar las posibilidades aportadas por las diferentes t\u00e9cnicas de acoplamiento entre modelos atmosf\u00e9ricos, de oleaje y oce\u00e1nicos. En \u00e9l se describe el modelo ecawom (european coupled atmosphere wave ocean model) as\u00ed como su aplicaci\u00f3n al estudio de un periodo tormentoso.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Simulacion numerica de procesos oceanograficos en las costas atlanticas espa\u00f1olas.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Simulacion numerica de procesos oceanograficos en las costas atlanticas espa\u00f1olas. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Enrique \u00e1lvarez Fanjul <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Alcal\u00e1<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1998<\/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> Ruiz De Elvira Antonio<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal:  Ortiz Bevia Mar\u00eda  Jose <\/li>\n<li>Jordi Font (vocal)<\/li>\n<li>Josep Llu\u00eds Pelegr\u00ed Llopart (vocal)<\/li>\n<li>Roger Flather (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Enrique \u00e1lvarez Fanjul El objetivo de esta tesis es estudiar, en las aguas atl\u00e1nticas espa\u00f1olas, la circulaci\u00f3n [&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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