{"id":1382,"date":"1994-01-01T00:00:00","date_gmt":"1994-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/1994\/01\/01\/determinacion-de-estructuras-atmosfericas-acopladas-a-la-precipitacion-local\/"},"modified":"1994-01-01T00:00:00","modified_gmt":"1994-01-01T00:00:00","slug":"determinacion-de-estructuras-atmosfericas-acopladas-a-la-precipitacion-local","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/determinacion-de-estructuras-atmosfericas-acopladas-a-la-precipitacion-local\/","title":{"rendered":"Determinacion de estructuras atmosfericas acopladas a la precipitacion local"},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Garcia Legaz Martinez Carlos <\/strong><\/h2>\n<p>Los objetivos pretendidos con la realizacion de la tesis se han centrado en el analisis de las variaciones de la precipitacion en la comunidad autonoma de Madrid y en la descripcion de los forzamientos termodinamicos asociados a ellas, junto con la identificacion y clasificacion de los acoplamientos atmosfera-superficie y la evaluacion del grado o intensidad de estos para, una vez efectuadas, aplicar la metodolog\u00eda resultante a escala regional. Como resultado se han encontrado tres estructuras coherentes representativas del modo de variacion de la precipitacion sobre el dominio espacial elegido durante el periodo de estudio. Asimismo se han investigado detalladamente las estructuras atmosfericas asociadas a las configuraciones de precipitacion mediante el analisis de la estructura dinamica y de inestabilidad termodinamica. Como resultado general se ha establecido una metodolog\u00eda clara y profunda sobre la que pueden basarse analisis de climatolog\u00eda termodinamica troposferica.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Determinacion de estructuras atmosfericas acopladas a la precipitacion local<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Determinacion de estructuras atmosfericas acopladas a la precipitacion local <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Garcia Legaz Martinez Carlos <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1994<\/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: Jose Agular Peris <\/li>\n<li>Pedro Sancho Diez (vocal)<\/li>\n<li>Vicente Quesada Paloma (vocal)<\/li>\n<li>Moises Egido Manzano (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Garcia Legaz Martinez Carlos Los objetivos pretendidos con la realizacion de la tesis se han centrado en [&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":[950,27,5952,5951,429],"tags":[5954,5953,5955,5957,5956,3367],"class_list":["post-1382","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-atmosfera","category-ciencias-de-la-tierra-y-del-espacio","category-estructura-atmosferica","category-mesometeorologia","category-meteorologia","tag-francisco-valero-rodriguez","tag-garcia-legaz-Martinez-carlos","tag-jose-agular-peris","tag-moises-egido-manzano","tag-pedro-sancho-diez","tag-vicente-quesada-paloma"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/1382","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=1382"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/1382\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=1382"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=1382"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=1382"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}