{"id":20293,"date":"2002-02-12T00:00:00","date_gmt":"2002-02-12T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/caracterizacion-de-parametros-turbulentos-en-una-zona-costera\/"},"modified":"2002-02-12T00:00:00","modified_gmt":"2002-02-12T00:00:00","slug":"caracterizacion-de-parametros-turbulentos-en-una-zona-costera","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/caracterizacion-de-parametros-turbulentos-en-una-zona-costera\/","title":{"rendered":"Caracterizaci\u00f3n de par\u00e1metros turbulentos en una zona costera"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Bego\u00f1a Ace\u00f1a Moreno <\/strong><\/h2>\n<p>Esta memoria se centra esencialmente en el estudio de los par\u00e1metros que caracterizan el estado turbulento de la baja atm\u00f3sfera en una zona costera y que son importantes datos de entrada en los modelos de dispersi\u00f3n de contaminantes y, por tanto, para calcular la concentraci\u00f3n (distribuci\u00f3n espacial y temporal), y dep\u00f3sito de los contaminantes. El problema que surge con las relaciones emp\u00edricas utilizadas en turbulencia es que est\u00e1n basadas en un limitado n\u00famero de datos experimentales.  muchas de estas relaciones se han obtenido con datos correspondientes a d\u00edas y en el mejor de los casos, pero en menor n\u00famero, a pocas semanas y, principalmente, en terrenos llanos. Por tanto, su representatividad y consecuentemente la validez del uso de estas relaciones, especialmente sobre terreno no llano y no homog\u00e9nero, como es el caso de zonas costeras, es cuestionable.  la pen\u00ednsula ib\u00e9rica, debido a su situaci\u00f3n geogr\u00e1fica, topograf\u00eda y tipo de cubierta vegetal, posee una serie de elementos diferenciales que la marcan espec\u00edficamente en el contexto europeo. Adem\u00e1s, una parte importante del territorio espa\u00f1ol corresponde a zonas costeras con una orograf\u00eda accidentada, por lo que la dispersi\u00f3n en estas zonas resulta extremadamente compleja.  el estudio realizado en esta memoria, se ha llevado a cabo utilizando los datos obtenidos en dos torres meteorol\u00f3gicas instaladas en la localidad de palomares (almer\u00eda), al sur de la pen\u00ednsula ib\u00e9rica, en la costa mediterr\u00e1nea (cap\u00edtulos ii y iii).  los par\u00e1metros turbulentos estudiados corresponden a la rugosidad local del terreno z0, a la velocidad de fricci\u00f3n u* (cap\u00edtulos iv y v) y, a los par\u00e1metros que definen la intensidad de turbulencia y su influencia en el c\u00e1lculo de la concentraci\u00f3n de un determinado contaminante emitido a la atm\u00f3sfera (cap\u00edtulo vi).  en el cap\u00edtulo i se describen brevemente las bases te\u00f3ricas desarrolladas para la capa superficial y en las qu<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Caracterizaci\u00f3n de par\u00e1metros turbulentos en una zona costera<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Caracterizaci\u00f3n de par\u00e1metros turbulentos en una zona costera <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Bego\u00f1a Ace\u00f1a Moreno <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 02\/12\/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> Cano Marchante Jos\u00e9 Leandro<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: emiliano Hern\u00e1ndez mart\u00edn <\/li>\n<li>Antonio Bru espino (vocal)<\/li>\n<li>Carlos Yag\u00ed\u00bce anguis (vocal)<\/li>\n<li>magdalena Palacios g\u00f3mez (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Bego\u00f1a Ace\u00f1a Moreno Esta memoria se centra esencialmente en el estudio de los par\u00e1metros que caracterizan el [&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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