{"id":28827,"date":"2018-03-09T09:21:41","date_gmt":"2018-03-09T09:21:41","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/interaccion-entre-escalas-en-la-variabilidad-climatica\/"},"modified":"2018-03-09T09:21:41","modified_gmt":"2018-03-09T09:21:41","slug":"interaccion-entre-escalas-en-la-variabilidad-climatica","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/alcala\/interaccion-entre-escalas-en-la-variabilidad-climatica\/","title":{"rendered":"Interaccion entre escalas en la variabilidad climatica."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Alvarez Garcia Francisco Jose <\/strong><\/h2>\n<p>La tesis aborda el problema de la interacci\u00f3n entre las escalas interanual, estacional y decadal en la variabilidad clim\u00e1tica de la regi\u00f3n tropical del pac\u00edfico, en datos de una simulaci\u00f3n con el modelo acoplado oc\u00e9ano &#8211; atm\u00f3sfera orca-echam4, conectados por la interfaz oasis.  la configuraci\u00f3n del experimento es global, con una resoluci\u00f3n horizontal de 2\u00c2\u00bax(1.5\u00c2\u00ba-0.5\u00c2\u00ba) en el oc\u00e9ano y aproximadamente 3.75\u00c2\u00bax3.75\u00c2\u00ba en la atm\u00f3sfera (truncamiento t30 en una aproximaci\u00f3n espectral). En su  ejecuci\u00f3n no fueron aplicadas correcciones de flujo, salvo por un per\u00edodo de inicializaci\u00f3n previo y por la restauraci\u00f3n, a lo largo de toda la simulaci\u00f3n, de la cubierta de hielo marino a valores climatol\u00f3gicos.  en este trabajo se analizan anomal\u00edas mensuales de las variables que describen el sistema oc\u00e9ano-atm\u00f3sfera en el pac\u00edfico tropical (temperatura de la superficie marina, presi\u00f3n atmosf\u00e9rica al nivel del mar, esfuerzos del viento, energ\u00eda t\u00e9rmica almacenada en la capa superior del oc\u00e9ano, corrientes horizontales, afloramiento, profundidad de la termoclina) en un intervalo simulado de cien a\u00f1os.  el fen\u00f3meno dominante en la variabilidad clim\u00e1tica del dominio estudiado es el  ni\u00f1o &#8211; oscilaci\u00f3n del sur, caracter\u00edstico de la banda interanual. este modo de variabilidad presenta una diversidad de comportamientos, tanto en las observaciones como en la simulaci\u00f3n estudiada; a partir de los datos proporcionados por esta \u00faltima, se establece una clasificaci\u00f3n de los episodios c\u00e1lidos y fr\u00edos que se producen en ella. La metodolog\u00eda de clasificaci\u00f3n es esencialmente un an\u00e1lisis de clusters o conglomerados, con un dise\u00f1o espec\u00edfico para la investigaci\u00f3n que se lleva a cabo.  del an\u00e1lisis de los mecanismos f\u00edsicos que subyacen a la clasificaci\u00f3n obtenida, se derivan resultados y conclusiones relativos a:  1) la intervenci\u00f3n y el modo de operar de los distintos modelos conceptuales (el oscilador retardado, el os<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Interaccion entre escalas en la variabilidad climatica.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Interaccion entre escalas en la variabilidad climatica. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Alvarez Garcia Francisco Jose <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Alcal\u00e1<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 24\/02\/2004<\/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> Ortiz Bebia Mar\u00eda  Jose<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal:  Diaz diaz Jes\u00fas idelfonso <\/li>\n<li>william Cabos narvaez (vocal)<\/li>\n<li>Rafael Bravo de la parra (vocal)<\/li>\n<li>josep llu\u00eds Pelegr\u00ed llopart (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Alvarez Garcia Francisco Jose La tesis aborda el problema de la interacci\u00f3n entre las escalas interanual, estacional [&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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