{"id":26415,"date":"2018-03-09T09:18:14","date_gmt":"2018-03-09T09:18:14","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/reanalisis-atmosferico-pluridecenal-de-alta-resolucion-en-la-cuenca-mediterranea\/"},"modified":"2018-03-09T09:18:14","modified_gmt":"2018-03-09T09:18:14","slug":"reanalisis-atmosferico-pluridecenal-de-alta-resolucion-en-la-cuenca-mediterranea","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/reanalisis-atmosferico-pluridecenal-de-alta-resolucion-en-la-cuenca-mediterranea\/","title":{"rendered":"Rean\u00e1lisis atmosf\u00e9rico pluridecenal de alta resoluci\u00f3n en la cuenca mediterr\u00e1nea"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Marcos Garc\u00eda Sotillo <\/strong><\/h2>\n<p>Con el fin de producir una base de datos atmosf\u00e9rica pluridecenal (1958-2001) de alta resoluci\u00f3n espacio-temporal centrada en la cuenca mediterr\u00e1nea se ha realizado un downscaling din\u00e1mico a partir de los datos de rean\u00e1lisis global ncep. Para llevar a cabo el downscaling se emple\u00f3 el modelo de \u00e1rea limitada remo junto con una t\u00e9cnica de nudging espectral. Se ha evaluado la sensibilidad del viento superficial simulado por remo a cambios en el par\u00e1metro de rugosidad superficial sobre mar y tierra y al forzamiento de la simulaci\u00f3n mediante rean\u00e1lisis era 15 en vez de ncep. La aplicaci\u00f3n remo ha sido validada exhaustivamente. Para ello se realizaron comparaciones entre diferentes par\u00e1metros superficiales y datos observacionales de sat\u00e9lite (escater\u00f3metro ers- 1\/2) y de estaciones, tanto offshore como terrestre. adem\u00e1s, se comprob\u00f3 por medio de comparaciones an\u00e1logas con los rean\u00e1lisis ncep la mejora introducida por el downscaling, poni\u00e9ndose de relieve el alto potencial que posee dicha t\u00e9cnica para la creaci\u00f3n de bases de datos de calidad en escala regional. Asimismo, ciertas variables superficiales remo (presi\u00f3n superficial y viento al nivel de 10 metros) han sido empleadas como forzamiento de modelos oceanogr\u00e1ficos. La validaci\u00f3n de estas aplicaciones oceanogr\u00e1ficas frente a observaciones de oleaje y nivel de mar han permitido realizar la validaci\u00f3n \u00abindirecta\u00bb de los campos remo empleados como forzamiento atmosf\u00e9rico. Una vez verificada sobre zonas mar\u00edtimas la calidad del viento simulado, se realiz\u00f3 una evaluaci\u00f3n de la variabilidad temporal del mismo a lo largo de 44 a\u00f1os, con especial \u00e9nfasis  en la evoluci\u00f3n del viento extremo. Se verific\u00f3 la idoneidad de los datos remo para la caracterizaci\u00f3n de episodios de viento extremo as\u00ed como la existencia de tendencias clim\u00e1ticas del viento obtenido a partir del downscaling. Estas tendencias han sido a su vez comparadas con las obtenidas a partir de los rean\u00e1<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Rean\u00e1lisis atmosf\u00e9rico pluridecenal de alta resoluci\u00f3n en la cuenca mediterr\u00e1nea<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Rean\u00e1lisis atmosf\u00e9rico pluridecenal de alta resoluci\u00f3n en la cuenca mediterr\u00e1nea <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Marcos Garc\u00eda Sotillo <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 22\/10\/2003<\/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 Rodr\u00edguez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: manuel Rego fern\u00e1ndez <\/li>\n<li>ralf Weisse (vocal)<\/li>\n<li>climent Ramis noguera (vocal)<\/li>\n<li>enrique \u00e1lvarez fanjul (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Marcos Garc\u00eda Sotillo Con el fin de producir una base de datos atmosf\u00e9rica pluridecenal (1958-2001) 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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