{"id":95726,"date":"2018-03-11T10:15:45","date_gmt":"2018-03-11T10:15:45","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/patrones-de-circulacion-oceanica-en-el-litoral-espanol\/"},"modified":"2018-03-11T10:15:45","modified_gmt":"2018-03-11T10:15:45","slug":"patrones-de-circulacion-oceanica-en-el-litoral-espanol","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/analisis-numerico\/patrones-de-circulacion-oceanica-en-el-litoral-espanol\/","title":{"rendered":"Patrones de circulaci\u00f3n oce\u00e1nica en el litoral espa\u00f1ol"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Mar\u00eda Liste Mu\u00f1oz <\/strong><\/h2>\n<p>En esta tesis, se ha desarrollado el modelo medina, que simula la circulaci\u00f3n oce\u00e1nica tridimensiional del atl\u00e1ntico norte y del mar mediterr\u00e1neo y da como resultado series temporales de salinidad, temperatura y componente u, v y w de la velocidad. Mediante la ejecuci\u00f3n de dicho modelo, se han generado 46 a\u00f1os de datos que se han validado mediante la comparaci\u00f3n de los mismos con una base de datos de climatolog\u00edas (gdp), adem\u00e1s de mediante el c\u00e1lculo del transporte en los principales canales y estrechos de la cuenca occidental mediterr\u00e1nea y del golfo de m\u00e9xico. Una vez que se han validado los resultados se ha demostrado adem\u00e1s, la capacidad que tiene el modelo medina para simular la formaci\u00f3n y la propagaci\u00f3n de la masa de agua mow (mediterranean overflow water ) y se ha conseguido demostrar que los modelos-z, como el modelo medina, son capaces de simular adecuadamente las corrientes de densidad, como por ejemplo la mow (dietrich et al., 2008). Por \u00faltimo se han aplicado dos herramientas estad\u00edsticas para el an\u00e1lisis de los resultados; la primera de ellas es la t\u00e9cnica estad\u00edstica est\u00e1ndar, an\u00e1lisis de componentes principales, tambi\u00e9n denominada an\u00e1lisis de funciones ortogonales emp\u00edricas (emprirical orthogonal function, eof), y la segunda son las redes neuronales auto-organizativas (self organizing maps, som). Se ha demostrado que tanto los eof como las som, adem\u00e1s de ser potentes herramientas estad\u00edsticas, son adecuadas para estudiar en este caso, las series temporales de variables oceanogr\u00e1ficas obtenidas a partir del modelo medina, con el fin de obtener patrones de circulaci\u00f3n, as\u00ed como la relaci\u00f3n de \u00e9stos con los patrones atmosf\u00e9ricos.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Patrones de circulaci\u00f3n oce\u00e1nica en el litoral espa\u00f1ol<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Patrones de circulaci\u00f3n oce\u00e1nica en el litoral espa\u00f1ol <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Mar\u00eda Liste Mu\u00f1oz <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Cantabria<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 30\/07\/2009<\/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: i\u00f1igo Losada rodriguez <\/li>\n<li>Manuel Espino infantes (vocal)<\/li>\n<li>bego\u00f1a Tejedor alvarez (vocal)<\/li>\n<li>alejandro Orfila f\u00ed\u00b6rster (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Mar\u00eda Liste Mu\u00f1oz En esta tesis, se ha desarrollado el modelo medina, que simula la circulaci\u00f3n oce\u00e1nica [&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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