{"id":35857,"date":"1998-01-01T00:00:00","date_gmt":"1998-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/medidas-espectrorradiometricas-para-la-determinacion-de-componentes-atmosfericos-ozono-vapor-de-agua-y-aerosoles-y-modelizacion-del-intercambio-radiativo-en-la-atmosfera\/"},"modified":"1998-01-01T00:00:00","modified_gmt":"1998-01-01T00:00:00","slug":"medidas-espectrorradiometricas-para-la-determinacion-de-componentes-atmosfericos-ozono-vapor-de-agua-y-aerosoles-y-modelizacion-del-intercambio-radiativo-en-la-atmosfera","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/medidas-espectrorradiometricas-para-la-determinacion-de-componentes-atmosfericos-ozono-vapor-de-agua-y-aerosoles-y-modelizacion-del-intercambio-radiativo-en-la-atmosfera\/","title":{"rendered":"Medidas espectrorradiometricas para la determinacion de componentes atmosfericos (ozono, vapor de agua y aerosoles) y modelizacion del intercambio radiativo en la atmosfera."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Plinio Duran Garcia <\/strong><\/h2>\n<p>En esta tesis se ha realizado un estudio sobre la determinaci\u00f3n y an\u00e1lisis de la evoluci\u00f3n de dos de los m\u00e1s importantes constituyentes atmosf\u00e9ricos: ozono y vapor de agua as\u00ed como la caracterizaci\u00f3n tanto de las propiedades f\u00edsicas como radiativas de los aerosoles sobre la vertical del punto de medida. Estas determinaciones est\u00e1n basadas en la medida y modelizaci\u00f3n de la componente directa de la radiaci\u00f3n solar espectral en el rango 300-1100 nm.  a su vez se ha desarrollado y validado su modelo de transferencia radiativo a \u00abdos flujos\u00bb que nos permite estimar las tres componentes de la radiaci\u00f3n directa, difusa y global, a nivel de suelo. Su aplicaci\u00f3n al c\u00e1lculo de la reflectancia de la atm\u00f3sfera nos permite una gran fiabilidad de dicha estimaci\u00f3n al estar basado en la propia validaci\u00f3n de la transmitancia de la atm\u00f3sfera a nivel de suelo. A su vez a esta se a\u00f1ade la medida de la reflectancia del suelo y diferentes cubiertas vegetales lo que presenta una gran aplicaci\u00f3n en el campo agroforestal.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Medidas espectrorradiometricas para la determinacion de componentes atmosfericos (ozono, vapor de agua y aerosoles) y modelizacion del intercambio radiativo en la atmosfera.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Medidas espectrorradiometricas para la determinacion de componentes atmosfericos (ozono, vapor de agua y aerosoles) y modelizacion del intercambio radiativo en la atmosfera. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Plinio Duran Garcia <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Valladolid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1998<\/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>Victoria Eugenia Cachorro Revilla<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal:  Frutos Baraja Angel M. De <\/li>\n<li>Manuel Gil Ojeda (vocal)<\/li>\n<li>Jos\u00e9 Antonio Mart\u00ednez Lozano (vocal)<\/li>\n<li>Manuel Lopez Puertas (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Plinio Duran Garcia En esta tesis se ha realizado un estudio sobre la determinaci\u00f3n y an\u00e1lisis 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 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":[950,27,27612,11575,12451],"tags":[95364,27614,63605,85172,95363,27616],"class_list":["post-35857","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-atmosfera","category-ciencias-de-la-tierra-y-del-espacio","category-optica-atmosferica","category-transferencia-radiactiva","category-valladolid","tag-frutos-baraja-angel-m-de","tag-jose-antonio-Martinez-lozano","tag-manuel-gil-ojeda","tag-manuel-lopez-puertas","tag-plinio-duran-garcia","tag-victoria-eugenia-cachorro-revilla"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/35857","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=35857"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/35857\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=35857"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=35857"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=35857"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}