{"id":86035,"date":"2018-03-10T00:10:33","date_gmt":"2018-03-10T00:10:33","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/aspectos-de-la-variabilidad-de-mesoescala-de-la-circulacion-marina-en-la-plataforma-continental-catalana\/"},"modified":"2018-03-10T00:10:33","modified_gmt":"2018-03-10T00:10:33","slug":"aspectos-de-la-variabilidad-de-mesoescala-de-la-circulacion-marina-en-la-plataforma-continental-catalana","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/aspectos-de-la-variabilidad-de-mesoescala-de-la-circulacion-marina-en-la-plataforma-continental-catalana\/","title":{"rendered":"Aspectos de la variabilidad de mesoescala de la circulaci\u00f3n marina en la plataforma continental catalana."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Pedro Antonio Arnau Del Amo <\/strong><\/h2>\n<p>Se ha desarrollado una investigaci\u00f3n de la estructura y la variabilidad de mesoescala de la circulaci\u00f3n marina en el sector norte de la plataforma continental catalana haciendo uso de t\u00e9cnicas de observaci\u00f3n in situ y remotas.  para llevar a cabo este estudio se realizaron cuatro campa\u00f1as oceanogr\u00e1ficas: la campa\u00f1a meca 93 en junio de 1993, la campa\u00f1a meca 95 en noviembre de 1995, la campa\u00f1a meca 96 en septiembre de 1996 y la campa\u00f1a meca 97 en noviembre de 1997. Durante las campa\u00f1as meca 93 y meca 95 se lanzaron boyas langrangianas argos y en 1993 se realiz\u00f3 un fondeo de dos corrent\u00edmetros en el \u00e1rea del ca\u00f1\u00f3n de blanes. Esta informaci\u00f3n de campo se ha complementado con secuencias multitemporales de im\u00e1genes noaa\/avhrr adquiridas durante el periodo comprendido entre 1993 y 1997. Finalmente se han empleado dos series temporales de datos complementarios, una serie de vientos adquirida en cap bear(1995-1997) y una serie de descargas medias diarias del r\u00edo r\u00f3dano(1960-1995).  como resultado del an\u00e1lisis de este volumen de informaci\u00f3n se ha podido mejorar el conocimiento de la circulaci\u00f3n de mesoescala en el \u00e1mbito de estudio. Una de las conclusiones de m\u00e1s interes es que la circulaci\u00f3n se encuentra muy influida por la advecci\u00f3n \u00abrecurrente\u00bb de remolinos anticicl\u00f3nicos a lo largo del litoral catal\u00e1n durante todas las estaciones del a\u00f1o. Dichos remolinos tienen un di\u00e1metro del orden de 30 millas n\u00e1uticas y se desplazan a una velocidad de 5 cm\/s. El lapso que transcurre entre&#8230;.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Aspectos de la variabilidad de mesoescala de la circulaci\u00f3n marina en la plataforma continental catalana.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Aspectos de la variabilidad de mesoescala de la circulaci\u00f3n marina en la plataforma continental catalana. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Pedro Antonio Arnau Del Amo <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Polit\u00e9cnica de catalunya<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 17\/07\/2000<\/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>Marcial Garc\u00eda L\u00f3pez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: manuel Cant\u00f3n garb\u00edn <\/li>\n<li>josep llu\u00eds Pelegr\u00ed llopart (vocal)<\/li>\n<li>Antonio Calafat frau (vocal)<\/li>\n<li>dami\u00ed\u00a0 Gomis bosch (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Pedro Antonio Arnau Del Amo Se ha desarrollado una investigaci\u00f3n de la estructura y la variabilidad de [&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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