{"id":139633,"date":"2026-01-12T17:47:18","date_gmt":"2026-01-12T17:47:18","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/los-mapas-de-estabilidad-de-estratificacion-y-la-prediccion-de-lluvias-copiosas\/"},"modified":"2026-01-12T17:47:18","modified_gmt":"2026-01-12T17:47:18","slug":"los-mapas-de-estabilidad-de-estratificacion-y-la-prediccion-de-lluvias-copiosas","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/los-mapas-de-estabilidad-de-estratificacion-y-la-prediccion-de-lluvias-copiosas\/","title":{"rendered":"Los mapas de estabilidad de estratificacion y la prediccion de lluvias copiosas"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Bernardino Garcia Sanchez <\/strong><\/h2>\n<p>Partiendo de la ecuacion de rossby y del teorema del torbellino de ertel, expresa la invariante de ertel-rossby en funcion del producto de dos magnitudes:  la vorticidad absoluta por la estabilidad de estratificacion de la atmosfera. Justifica que la primera magnitud es de caracter dinamico y horizontal y la segunda de caracter termodinamico y vertical. Utiliza las energias estaticas seca y humeda para determinar las estabilidades de estratificacion baricas, o sea, usa la presion como coordenada vertical. Destaca la importancia del termino termodinamico para la prediccion a nivel de mesoescala. Para ello, analiza 62 situaciones meteorologicas reales de los a\u00f1os 1989 y 1990, trazando los mapas de estabilidad correspondientes. Para cada mapa calcula las estabilidades de estratificacion de unas 40 columnas atmosfericas.  muestra teorica y practicamente que las precipitaciones copiosas ocurren en las zonas de minima estabilidad, o de adveccion de columnas de menores estabilidades.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Los mapas de estabilidad de estratificacion y la prediccion de lluvias copiosas<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Los mapas de estabilidad de estratificacion y la prediccion de lluvias copiosas <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Bernardino Garcia Sanchez <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Salamanca<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1992<\/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>Jose Garmendia Iraundegui<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Jose Barcala Herrero <\/li>\n<li>Carlos Santamaria Salazar (vocal)<\/li>\n<li> Sevilla De Lerma Miguel J. (vocal)<\/li>\n<li>Jes\u00fas Seco Santos (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Bernardino Garcia Sanchez Partiendo de la ecuacion de rossby y del teorema del torbellino de ertel, expresa [&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":[950,27,5951,429,9386,9683],"tags":[237326,9687,6652,9686,9685,50254],"class_list":["post-139633","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-atmosfera","category-ciencias-de-la-tierra-y-del-espacio","category-mesometeorologia","category-meteorologia","category-salamanca","category-termodinamica-atmosferica","tag-bernardino-garcia-sanchez","tag-carlos-santamaria-salazar","tag-jesus-seco-santos","tag-jose-barcala-herrero","tag-jose-garmendia-iraundegui","tag-sevilla-de-lerma-miguel-j"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/139633","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=139633"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/139633\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=139633"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=139633"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=139633"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}