{"id":142676,"date":"1993-01-01T00:00:00","date_gmt":"1993-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/variacion-espacial-y-temporal-de-los-parametros-de-estabilidad-en-orografia-compleja-y-ondas-de-montana\/"},"modified":"1993-01-01T00:00:00","modified_gmt":"1993-01-01T00:00:00","slug":"variacion-espacial-y-temporal-de-los-parametros-de-estabilidad-en-orografia-compleja-y-ondas-de-montana","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/variacion-espacial-y-temporal-de-los-parametros-de-estabilidad-en-orografia-compleja-y-ondas-de-montana\/","title":{"rendered":"Variacion espacial y temporal de los parametros de estabilidad en orografia compleja y ondas de monta\u00f1a."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Julio Diaz Jimenez <\/strong><\/h2>\n<p>Cuando un flujo de aire atraviesa un obstaculo monta\u00f1oso se originan una serie de fenomenos a mesoescala tales como vortices a sotavento, ondas de monta\u00f1a e inestabilidades atmosfericas que dan lugar a la formacion de dipolos orograficos con caracteristicas no bien determinadas y de gran trascendencia en meteorolog\u00eda. La presente memoria es un aporte al conocimiento de los fenomenos antes mencionados. Para ello se ha seguido la metodolog\u00eda de un desarrollo teorico, un proceso experimental y una posterior comprobacion de los fenomenos, que siendo conocidos en modelos de laboratorio y mediante simulaciones numericas no se habian constatado en la realidad.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Variacion espacial y temporal de los parametros de estabilidad en orografia compleja y ondas de monta\u00f1a.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Variacion espacial y temporal de los parametros de estabilidad en orografia compleja y ondas de monta\u00f1a. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Julio Diaz Jimenez <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1993<\/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>Emiliano Hern\u00e1ndez Mart\u00edn<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Cristobal Fernandez Pineda <\/li>\n<li> Pacheco Castelao Jos\u00e9 Miguel (vocal)<\/li>\n<li>Pedro Sancho Diaz (vocal)<\/li>\n<li>Moises Egido Manzano (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Julio Diaz Jimenez Cuando un flujo de aire atraviesa un obstaculo monta\u00f1oso se originan una serie de [&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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