{"id":34352,"date":"1998-01-01T00:00:00","date_gmt":"1998-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/modelo-de-prediccion-de-la-precipitacion-peninsular-en-climas-perturbados\/"},"modified":"1998-01-01T00:00:00","modified_gmt":"1998-01-01T00:00:00","slug":"modelo-de-prediccion-de-la-precipitacion-peninsular-en-climas-perturbados","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/modelo-de-prediccion-de-la-precipitacion-peninsular-en-climas-perturbados\/","title":{"rendered":"Modelo de prediccion de la precipitacion peninsular en climas perturbados."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Fidel Gonzalez Rouco <\/strong><\/h2>\n<p>En este trabajo se crea, en primer lugar, una base de datos de alta resoluci\u00f3n de la precipitaci\u00f3n peninsular a escala mensual para el per\u00edodo 1899-1989 introduciendo un an\u00e1lisis de control de calidad que involucra t\u00e9cnicas optimizadas de correcci\u00f3n de datos an\u00f3malos, homegeneizaci\u00f3n e interpolaci\u00f3n de datos inexistentes.  asimismo, se analiza la variabilidad espaciotemporal a escala anual, interdecenal y secular de la precipitaci\u00f3n peninsular y de las presiones medias a nivel del mar en el atl\u00e1ntico norte. Este estudio se combina con fines de validaci\u00f3n, con las simulaciones respectivas del modelo clim\u00e1tico del hadley centre.  por otra parte, se formula un modelo emp\u00edrico estad\u00edstico de proyecci\u00f3n regional de las salidas del modelo clim\u00e1tico sobre la pen\u00ednsula ib\u00e9rica. Esto ha permitido detectar nuevos modos de variabilidad clim\u00e1tica acoplada entre ambas escalas espaciales.  se han estudiado las relaciones entre escalas en condiciones de clima perturbado utilizando integraciones con forzamiento radiativo por aumento de gases invernadero y aerosoles, confirm\u00e1ndose su invarianza.  finalmente, se han proyectado las simulaciones de las presiones medias a nivel del mar en condiciones de clima perturbado utilizando el modelo estad\u00edstico para obtener la respuesta de la precipitaci\u00f3n peninsular a dicho forzamiento. Los resultados se comparan con las tendencias observadas.  p. Clave: clima, cambio clim\u00e1tico, variabilidad clim\u00e1tica, precipitaci\u00f3n mensual, pen\u00ednsula ib\u00e9rica, atl\u00e1ntico norte, modelos emp\u00edrico estad\u00edsticos, proyecciones regionales (downscaling), homogeneizaci\u00f3n.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Modelo de prediccion de la precipitacion peninsular en climas perturbados.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Modelo de prediccion de la precipitacion peninsular en climas perturbados. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Fidel Gonzalez Rouco <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/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>Francisco Valero Rodriguez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Manuel Rego Fernandez <\/li>\n<li>Felipe Fernandez Garcia (vocal)<\/li>\n<li> Luis Vazquez Martinez Luis (vocal)<\/li>\n<li> Garcia Legaz Martinez Carlos (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Fidel Gonzalez Rouco En este trabajo se crea, en primer lugar, una base de datos de alta [&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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