{"id":48944,"date":"2020-12-29T02:12:52","date_gmt":"2020-12-29T02:12:52","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/la-transicion-climatica-del-cantabrico-oriental-al-valle-medio-del-ebro\/"},"modified":"2020-12-29T02:12:52","modified_gmt":"2020-12-29T02:12:52","slug":"la-transicion-climatica-del-cantabrico-oriental-al-valle-medio-del-ebro","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/la-transicion-climatica-del-cantabrico-oriental-al-valle-medio-del-ebro\/","title":{"rendered":"La transicion climatica del cantabrico oriental al valle medio del ebro."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Eugenio Ruiz Urrestazu <\/strong><\/h2>\n<p>Segun los principios de la climatolog\u00eda dinamica  se establece una serie de tipos de tiempo en valores meteorologicos concretos con una triple vertiente barica termica y pluviometrica. Paralelamente  y como interaccion entre los metodos dinamico y sintetico  se especifica el alcance de la tecnica estadistica del analisis factorial aplicada al establecimiento de una comarcalizacion climatica. Las variadad fuentes empleadas cierran esta primera parte introductoria. Los resultados de los analisis factoriales de cada estacion se plasman en mapas que limitan las comarcas climaticas para cada epoca del a\u00f1o. Al final de cada una de estas se condensan los factores generales que las definen. Se concluyen con un resumen anual de los tipos de tiempo y de las comarcas surgidas en el conjunto del a\u00f1o.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>La transicion climatica del cantabrico oriental al valle medio del ebro.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 La transicion climatica del cantabrico oriental al valle medio del ebro. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Eugenio Ruiz Urrestazu <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Navarra<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1981<\/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>Alfredo Pablo Florist\u00e1n Im\u00edzcoz<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Alfredo Pablo Florist\u00e1n Im\u00edzcoz <\/li>\n<li>Antonio Higueras Arnal (vocal)<\/li>\n<li>Jose-manuel Casas Torres (vocal)<\/li>\n<li>Manuel Ferrer Regales (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Eugenio Ruiz Urrestazu Segun los principios de la climatolog\u00eda dinamica se establece una serie de tipos 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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