{"id":95,"date":"2013-04-19T07:43:17","date_gmt":"2013-04-19T07:43:17","guid":{"rendered":"https:\/\/smc.ihcantabria.es\/SMC25\/?page_id=95"},"modified":"2017-03-13T12:40:53","modified_gmt":"2017-03-13T12:40:53","slug":"mopla","status":"publish","type":"page","link":"https:\/\/smc.ihcantabria.es\/SMC25\/mopla\/","title":{"rendered":"Mopla"},"content":{"rendered":"<p><img loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-96 alignnone\" src=\"https:\/\/smc.ihcantabria.es\/SMC25\/wp-content\/uploads\/2013\/04\/logoMopla.gif\" alt=\"logoMopla\" width=\"200\" height=\"64\" \/><\/p>\n<p style=\"text-align: justify;\"><strong>Modelo de propagaci\u00f3n de Oleaje, corriente y evoluci\u00f3n morfodin\u00e1mica de PLAyas<\/strong><\/p>\n<p style=\"text-align: justify;\">El programa MOPLA, \u00abMorfodin\u00e1mica de playas\u00bb, permite simular la propagaci\u00f3n del oleaje desde profundidades indefinidas hasta la l\u00ednea de costa. A partir de este oleaje, se lleva a cabo el c\u00e1lculo de corrientes inducidas en la zona de rompientes, y finalmente, se simula la evoluci\u00f3n morfodin\u00e1mica de una playa.<\/p>\n<p style=\"text-align: justify;\">El MOPLA incluye los siguientes modelos:<\/p>\n<ul>\n<li style=\"text-align: justify;\"><b>Oluca:<\/b>\u00a0Modelo parab\u00f3lico de propagaci\u00f3n de oleaje (monocrom\u00e1tico y espectral).<\/li>\n<li style=\"text-align: justify;\"><b>Copla:<\/b>\u00a0Modelo de Corrientes en playas inducidas por la rotura del oleaje espectral.<\/li>\n<li style=\"text-align: justify;\"><b>Eros:<\/b>\u00a0Modelo de Erosi\u00f3n &#8211; sedimentaci\u00f3n y evoluci\u00f3n de la batimetr\u00eda en playas (debido al oleaje espectral).<\/li>\n<\/ul>\n<p style=\"text-align: center;\"><a href=\"https:\/\/smc.ihcantabria.es\/SMC25\/wp-content\/uploads\/2013\/04\/mopla.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-97 aligncenter\" src=\"https:\/\/smc.ihcantabria.es\/SMC25\/wp-content\/uploads\/2013\/04\/mopla-300x245.png\" alt=\"mopla\" width=\"300\" height=\"245\" srcset=\"https:\/\/smc.ihcantabria.es\/SMC25\/wp-content\/uploads\/2013\/04\/mopla-300x245.png 300w, https:\/\/smc.ihcantabria.es\/SMC25\/wp-content\/uploads\/2013\/04\/mopla.png 944w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><\/p>\n<p><\/p>","protected":false},"excerpt":{"rendered":"<p>Modelo de propagaci\u00f3n de Oleaje, corriente y evoluci\u00f3n morfodin\u00e1mica de PLAyas El programa MOPLA, \u00abMorfodin\u00e1mica de playas\u00bb, permite simular la propagaci\u00f3n del oleaje desde profundidades indefinidas hasta la l\u00ednea de costa. A partir de este oleaje, se lleva a cabo el c\u00e1lculo de corrientes inducidas en la zona de rompientes, y finalmente, se simula la [&hellip;]<\/p>\n","protected":false},"author":2,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"open","template":"","meta":{"footnotes":""},"class_list":["post-95","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/smc.ihcantabria.es\/SMC25\/wp-json\/wp\/v2\/pages\/95","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/smc.ihcantabria.es\/SMC25\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/smc.ihcantabria.es\/SMC25\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/smc.ihcantabria.es\/SMC25\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/smc.ihcantabria.es\/SMC25\/wp-json\/wp\/v2\/comments?post=95"}],"version-history":[{"count":10,"href":"https:\/\/smc.ihcantabria.es\/SMC25\/wp-json\/wp\/v2\/pages\/95\/revisions"}],"predecessor-version":[{"id":716,"href":"https:\/\/smc.ihcantabria.es\/SMC25\/wp-json\/wp\/v2\/pages\/95\/revisions\/716"}],"wp:attachment":[{"href":"https:\/\/smc.ihcantabria.es\/SMC25\/wp-json\/wp\/v2\/media?parent=95"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}