{"id":15962,"date":"2002-08-03T00:00:00","date_gmt":"2002-08-03T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/determinacion-de-las-propiedades-fisicas-y-radiactivas-de-aerosoles-atmosfericos-a-partir-de-medidas-de-extincion-de-la-radiacion-solar-a-nivel-del-suelo\/"},"modified":"2002-08-03T00:00:00","modified_gmt":"2002-08-03T00:00:00","slug":"determinacion-de-las-propiedades-fisicas-y-radiactivas-de-aerosoles-atmosfericos-a-partir-de-medidas-de-extincion-de-la-radiacion-solar-a-nivel-del-suelo","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/determinacion-de-las-propiedades-fisicas-y-radiactivas-de-aerosoles-atmosfericos-a-partir-de-medidas-de-extincion-de-la-radiacion-solar-a-nivel-del-suelo\/","title":{"rendered":"Determinaci\u00f3n de las propiedades fisicas y radiactivas de aerosoles atmosfericos a partir de medidas de extinci\u00f3n de la radiacion solar a nivel del suelo."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Roberto Pedros Esteban <\/strong><\/h2>\n<p>Los aerosoles atmosfericos son particulas microscopicas que se encuentran suspendidas en el aire y siguen el movimiento del mismo. El conocimiento de los aerosoles es complejo debido a su enorme variabilidad espacial y temporal y es importante por dos motivos:  -para conocer el forzamiento radiativo y sus efectos sobre el clima.  -para efectuar la correci\u00f3n atmosferica en im\u00e1genes de satelite  el objetivo de este trabajo ha sido determinar el espesor optico, la distribucion de tama\u00f1os, la funcion de fase y el albedo de dispersi\u00f3n simple de los aerosoles atmosfericos a partir de medidas de extinci\u00f3n de la radiacion solar.  para ello se ha realizado una serie de campa\u00f1as en Valencia y en barrax (albacete). En ellas se utilizo dos espectrorradiometros li-cor 1800 y optronic 754-0-pmt, asi como un fotometro microtops ii, que fueron caracterizados en el laboratorio antes de su utilizacion tambien se utiliz\u00f3 un lidar de retrodifusion aerotransportado para validar el procedimiento de obtenci\u00f3n del espesor optico.  con la instrumentaci\u00f3n y la metodolog\u00eda propuesta ha sido posible obtener las propiedades fisicas y radiativas antes mencionadas y asi identificar los aerosoles relacionandolos con las movimientos de las masas de aire en las 48 horas anteriores a la medida.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Determinaci\u00f3n de las propiedades fisicas y radiactivas de aerosoles atmosfericos a partir de medidas de extinci\u00f3n de la radiacion solar a nivel del suelo.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Determinaci\u00f3n de las propiedades fisicas y radiactivas de aerosoles atmosfericos a partir de medidas de extinci\u00f3n de la radiacion solar a nivel del suelo. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Roberto Pedros Esteban <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Universitat de val\u00e9ncia (estudi general)<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 08\/03\/2002<\/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 Antonio Mart\u00ednez Lozano<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Carlos Ferreira garcia <\/li>\n<li>Javier Ca\u00f1ada rivera (vocal)<\/li>\n<li>lucas Alados arboledas (vocal)<\/li>\n<li>jeronimo Lorente castello (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Roberto Pedros Esteban Los aerosoles atmosfericos son particulas microscopicas que se encuentran suspendidas en el aire y [&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":[950,27,199,1525,27612,50168,35505],"tags":[11734,2211,4332,27614,21757,50635],"class_list":["post-15962","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-atmosfera","category-ciencias-de-la-tierra-y-del-espacio","category-fisica","category-optica","category-optica-atmosferica","category-radiacion-visible","category-radiometria","tag-carlos-ferreira-garcia","tag-javier-canada-rivera","tag-jeronimo-lorente-castello","tag-jose-antonio-Martinez-lozano","tag-lucas-alados-arboledas","tag-roberto-pedros-esteban"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/15962","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=15962"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/15962\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=15962"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=15962"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=15962"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}