{"id":139914,"date":"2026-01-12T17:49:54","date_gmt":"2026-01-12T17:49:54","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/genesis-de-crecidas-en-pequenas-cuencas-semiaridas-barranc-de-carraixet-y-rambla-de-poyo\/"},"modified":"2026-01-12T17:49:54","modified_gmt":"2026-01-12T17:49:54","slug":"genesis-de-crecidas-en-pequenas-cuencas-semiaridas-barranc-de-carraixet-y-rambla-de-poyo","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/genesis-de-crecidas-en-pequenas-cuencas-semiaridas-barranc-de-carraixet-y-rambla-de-poyo\/","title":{"rendered":"\u00abgenesis de crecidas en peque\u00f1as cuencas semiaridas: barranc de carraixet y rambla de poyo\u00bb."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Ana Mar\u00eda Camarasa Belmonte <\/strong><\/h2>\n<p>A partir de los datos proporcionados por el sistema automatico de informacion hidrologica (saih), completados por los del servicio nacional de meteorolog\u00eda, el presente trabajo profundiza en los mecanismos de prevencion y formacion de avenidas en peque\u00f1as cuencas semiaridas tomando como base espacial dos ramblas mediterraneas: el barranc de carraixet y la rambla de poyo. En la tesis se pone de manifiesto la gran variabilidad espacio-temporal de la lluvia, cuya estructura horizontal muestra un patron celular jerarquizado muy mediatizado por el relieve. La respuesta de la cuenca es rapida, con grandes perdidas hidricas y formacion de frentes de ola moviles.  los ensayos de prediccion matematica de la crecida a partir del hidrograma unitario geomorfologico presentan resultados alentadores para este tipo de cuencas.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>\u00abgenesis de crecidas en peque\u00f1as cuencas semiaridas: barranc de carraixet y rambla de poyo\u00bb.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 \u00abgenesis de crecidas en peque\u00f1as cuencas semiaridas: barranc de carraixet y rambla de poyo\u00bb. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Ana Mar\u00eda Camarasa Belmonte <\/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 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>Joan Francesc Mateu Belles<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal:  Carles I Genoves Jose <\/li>\n<li>Vicente Fullana Serra (vocal)<\/li>\n<li>Vicen\u00ed\u00a7 M. Rossell\u00f3 Verger (vocal)<\/li>\n<li>Francisco Lopez Bermudez (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Ana Mar\u00eda Camarasa Belmonte A partir de los datos proporcionados por el sistema automatico de informacion hidrologica [&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":[27,5742,5741,13196,1666],"tags":[59002,254457,24919,14149,26821,16924],"class_list":["post-139914","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-ciencias-geograficas","category-geografia-fisica","category-hidrografia","category-hidrologia","tag-ana-maria-camarasa-belmonte","tag-carles-i-genoves-jose","tag-francisco-lopez-bermudez","tag-joan-francesc-mateu-belles","tag-viceni-m-rossello-verger","tag-vicente-fullana-serra"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/139914","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=139914"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/139914\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=139914"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=139914"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=139914"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}