{"id":11888,"date":"2001-03-07T00:00:00","date_gmt":"2001-03-07T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/desarrollo-y-validacion-de-un-procedimiento-digital-para-los-analisis-morfografocos\/"},"modified":"2001-03-07T00:00:00","modified_gmt":"2001-03-07T00:00:00","slug":"desarrollo-y-validacion-de-un-procedimiento-digital-para-los-analisis-morfografocos","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/desarrollo-y-validacion-de-un-procedimiento-digital-para-los-analisis-morfografocos\/","title":{"rendered":"Desarrollo y validaci\u00f3n de un procedimiento digital para los an\u00e1lisis morfogr\u00e1focos."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Sanz Santos Miguel Angel <\/strong><\/h2>\n<p>Esta tesis doctora desarrolla una metodolog\u00eda de an\u00e1lisis de la superficie terrestre, enfocada a la obtenci\u00f3n de par\u00e1metros fisiogr\u00e1ficos y geom\u00e9tricos de las formas constitutivas del territorio. Dicha metodolog\u00eda se basa en el tratamiento del modelo digital de elevaci\u00f3n y usa como par\u00e1metro fundamental la pendiente del terreno.  el tratamiento del modelo digital de elevaci\u00f3n da como resultado una serie de par\u00e1metros espec\u00edficos sobre la superficie del terreno, que desglosan el relieve en sus caracter\u00edsticas geom\u00e9tricas concretas. La recombinaci\u00f3n y ponderaci\u00f3n de cada uno de ellos con el resto permite realzar la fisonom\u00edas fundamentales; el nivel del detalle de esa fisonom\u00edas, estar\u00e1 siempre de acuerdo con la escala de trabajo, la precisi\u00f3n del modelo digital de elevaci\u00f3n y la jerarquizaci\u00f3n de los aspectos perceptivos que queremos resaltar.  toda esta simplificaci\u00f3n de la complejidad de la superficie del terreno se concreta en una cartograf\u00eda que desglosa los aspectos fundamentales del territorio (grupos morfom\u00e9tricos) y las subdivide en funci\u00f3n de cominaciones  de los par\u00e1metros (unidades morfom\u00e9tricas). A estas dos etapas de paroximaci\u00f3n, se le a\u00f1ade una tercera m\u00e1s centrada en el an\u00e1lisis de formas espec\u00edficas y singulares, completando el an\u00e1lisis.  la validaci\u00f3n del modelo, se ha realizado comparando la cartograf\u00eda obtenida mediante este el procedimiento con la elaborada seg\u00fan los m\u00e9todos tradicional. El resultado de la uni\u00f3n de ambas cartograf\u00edas permite obtener mayor precisi\u00f3n en los l\u00edmites de las formas del relieve, un tratamiento sistem\u00e1tico y generalizado para zonas de dif\u00edcil sobdivisi\u00f3n y clasificaci\u00f3n, a si como la caracterizaci\u00f3n y confirmaci\u00f3n de nuevas unidades morfol\u00f3gicas para el sistema central espa\u00f1ol.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Desarrollo y validaci\u00f3n de un procedimiento digital para los an\u00e1lisis morfogr\u00e1focos.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Desarrollo y validaci\u00f3n de un procedimiento digital para los an\u00e1lisis morfogr\u00e1focos. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Sanz Santos Miguel Angel <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 03\/07\/2001<\/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> Pedraza Gilsanz JavierDe<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: pedro emilio Martinez alfaro <\/li>\n<li>rosa Mar\u00eda Carrasco gonzalez (vocal)<\/li>\n<li>Rafael Escribano bomb\u00edn (vocal)<\/li>\n<li>\u00c1lvaro Garcia quintana (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Sanz Santos Miguel Angel Esta tesis doctora desarrolla una metodolog\u00eda de an\u00e1lisis de la superficie terrestre, enfocada [&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 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