{"id":40742,"date":"1999-01-01T00:00:00","date_gmt":"1999-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/propagacion-de-la-onda-de-marea-en-estuarios-someros\/"},"modified":"1999-01-01T00:00:00","modified_gmt":"1999-01-01T00:00:00","slug":"propagacion-de-la-onda-de-marea-en-estuarios-someros","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/propagacion-de-la-onda-de-marea-en-estuarios-someros\/","title":{"rendered":"Propagacion de la onda de marea en estuarios someros."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Pedro Lomonaco Tonda <\/strong><\/h2>\n<p>La deformaci\u00f3n de la onda de marea en aguas someras, producto de la diferencia de celeridades a lo largo del tiempo, lleva asociada una asimetr\u00eda en el campo de velocidades y, con \u00e9sta, una tendencia evolutiva de la configuraci\u00f3n morfol\u00f3gica del estuario. Se presenta un modelo anal\u00edtico capaz de reproducir la propagaci\u00f3n de la onda de marea en estuarios someros, as\u00ed como la generaci\u00f3n de las sobremareas, responsables de la deformaci\u00f3n de la onda y la asimetr\u00eda de las velocidades. Asimismo, se demuestra el efecto simult\u00e1neo de la configuraci\u00f3n de la secci\u00f3n transversal, en particular la presencia de los bajos mareales, las dimensiones del estuario y la fricci\u00f3n del fondo, en la recuperaci\u00f3n de la simetr\u00eda de las velocidades que conlleva, por lo tanto, la estabilidad del estuario. el an\u00e1lisis de sensibilidad de todos los par\u00e1metros representativos del estuario conduce a la elaboraci\u00f3n de un modelo conceptual que permite, de forma simplificada, la descripci\u00f3n completa del comportamiento de la onda de marea al propagarse por un estuario, incluyendo la generaci\u00f3n de sobremareas y, en consecuencia, definir su tendencia evolutiva.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Propagacion de la onda de marea en estuarios someros.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Propagacion de la onda de marea en estuarios someros. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Pedro Lomonaco Tonda <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Cantabria<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1999<\/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>Ra\u00fal Medina Santamar\u00eda<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Jos\u00e9 Antonio Revilla cortezon <\/li>\n<li>sebastia Montserrat tomas (vocal)<\/li>\n<li>marcial Garc\u00eda l\u00f3pez (vocal)<\/li>\n<li>bego\u00f1a Tejedor alvarez (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Pedro Lomonaco Tonda La deformaci\u00f3n de la onda de marea en aguas someras, producto de la diferencia [&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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