{"id":81183,"date":"1999-11-11T00:00:00","date_gmt":"1999-11-11T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/la-circulacion-atmosferica-euroatlantica-y-el-clima-de-pequenos-territorios-la-peninsula-iberica-y-catalunya\/"},"modified":"1999-11-11T00:00:00","modified_gmt":"1999-11-11T00:00:00","slug":"la-circulacion-atmosferica-euroatlantica-y-el-clima-de-pequenos-territorios-la-peninsula-iberica-y-catalunya","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/la-circulacion-atmosferica-euroatlantica-y-el-clima-de-pequenos-territorios-la-peninsula-iberica-y-catalunya\/","title":{"rendered":"La circulacion atmosferica euroatlantica y el clima de peque\u00f1os territorios. la peninsula iberica y catalunya."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Vazquez Lopez Luis Antonio <\/strong><\/h2>\n<p>Con el proposito general de la identificacion de relaciones a largo plazo entre la circulacion atmosferica extratropical del hemisferio norte y la distribucion de las anomalias de precipitacion en las grandes cuencas hidrologicas de la peninsula iberica y en catalunya, se ha implementado una metodolog\u00eda tipo \u00abdownscaline\u00bb, por medio de la cual se alcanza la identficacion de dos tipos de patrones de variabilidad, para invierno y oto\u00f1o, cada uno de los cuales vincula una combinaci\u00f3n de teleconexiones atmosfericas (nao, ea,eu-2, eu-1) de gran escala con un tipo de distribucion de anomalias de precipitacion regional. Las primeras soluciones discriminan condiciones de \u00abhumedad\u00bb y \u00absequedad\u00bb estaciones, las segundas tienen a diferenciar rasgos atlanticos de mediterraneos. Un modelo de regresion basado en las relaciones empirico-estadisticas obtenidas permite una estimaciion eficiente de las precipitaciones estacionales en gran parte de las cuencas ibericas. se ha utilizado extensamente el analisis de funciones ortogonales empiricas y el analisis de correlacion canonica, para el estudio de la variabilidad, la obtencion de las relaciones estadisticas y la aplicaci\u00f3n del modelo.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>La circulacion atmosferica euroatlantica y el clima de peque\u00f1os territorios. la peninsula iberica y catalunya.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 La circulacion atmosferica euroatlantica y el clima de peque\u00f1os territorios. la peninsula iberica y catalunya. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Vazquez Lopez Luis Antonio <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Barcelona<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 11\/11\/1999<\/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>Jos\u00e9 Miguel Raso Nadal<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: pedro Clavero paricio <\/li>\n<li> Llebot rabagliati josep enric (vocal)<\/li>\n<li>Jos\u00e9 Mar\u00eda Cuadrat prats (vocal)<\/li>\n<li>agust\u00ed Jans? clar (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Vazquez Lopez Luis Antonio Con el proposito general de la identificacion de relaciones a largo plazo entre [&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 center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"footnotes":""},"categories":[951,950,27,4329,4327,22619,41996],"tags":[26214,19612,66990,39871,80633,173368],"class_list":["post-81183","post","type-post","status-publish","format-standard","hentry","category-barcelona","category-ciencias-de-la-atmosfera","category-ciencias-de-la-tierra-y-del-espacio","category-climatologia","category-climatologia-regional","category-dinamica-atmosferica","category-microclimatologia","tag-agusti-jans-clar","tag-jose-maria-cuadrat-prats","tag-jose-miguel-raso-nadal","tag-llebot-rabagliati-josep-enric","tag-pedro-clavero-paricio","tag-vazquez-lopez-luis-antonio"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/81183","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/comments?post=81183"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/81183\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=81183"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=81183"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=81183"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}