{"id":2243,"date":"2025-10-31T12:15:00","date_gmt":"2025-10-31T11:15:00","guid":{"rendered":"https:\/\/www.ub.edu\/geomarines\/web\/?post_type=noticia&#038;p=2243"},"modified":"2026-06-18T13:29:13","modified_gmt":"2026-06-18T11:29:13","slug":"cascades-submarines-a-mes-de-1000-m-de-profunditat-prop-del-cap-de-creus-i-validacio-de-models-oceanics","status":"publish","type":"noticia","link":"https:\/\/www.ub.edu\/geomarines\/web\/noticia\/cascades-submarines-a-mes-de-1000-m-de-profunditat-prop-del-cap-de-creus-i-validacio-de-models-oceanics\/","title":{"rendered":"Cascades submarines a m\u00e9s de 1000 m de profunditat\u00a0prop\u00a0del Cap de Creus\u00a0i validaci\u00f3 de models oce\u00e0nics"},"content":{"rendered":"\n<p class=\"wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Les cascades submarines&nbsp;al&nbsp;nordoest&nbsp;del Mediterrani&nbsp;s\u00f3n episodis en qu\u00e8 l\u2019aigua propera a la costa, en hiverns freds i ventosos,&nbsp;es refreda prou com per enfonsar-se a gran velocitat fins a m\u00e9s de 2000 m, principalment&nbsp;seguint grans valls submarines que coneixem com a&nbsp;canyons submarins.&nbsp;Les&nbsp;estudiem&nbsp;mitjan\u00e7ant aparells lligats en un fondeig a 1000 metres de profunditat que mesuren corrents, temperatura i sediments en suspensi\u00f3;&nbsp;i&nbsp;amb dades&nbsp;de models&nbsp;oce\u00e0nics&nbsp;de&nbsp;Copernicus, que complementen&nbsp;la informaci\u00f3 de les&nbsp;mesures.&nbsp;En aquest article&nbsp;mostrem totes les cascades submarines profundes que hi ha hagut al fons del canyons submarins propers al Cap de Creus des de 1987,&nbsp;i&nbsp;demostrem&nbsp;com un model oce\u00e0nic \u00e9s capa\u00e7 de simular-les adequadament. Aquest fet significa un aven\u00e7 per al coneixement&nbsp;de&nbsp;la circulaci\u00f3 marina profunda&nbsp;ja que&nbsp;el models ens permeten reconstruir&nbsp;els corrents&nbsp;en zones&nbsp;i moments&nbsp;on les&nbsp;mesuresno&nbsp;son&nbsp;possibles,&nbsp;i mirar&nbsp;enrere en el temps&nbsp;diversos anys, permetent estudis clim\u00e0tics.&nbsp;<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>LINK<\/strong>:<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><a href=\"https:\/\/os.copernicus.org\/articles\/21\/2169\/2025\/os-21-2169-2025.html\"><\/a><a href=\"https:\/\/os.copernicus.org\/articles\/21\/2169\/2025\/os-21-2169-2025.html\" target=\"_blank\" rel=\"noreferrer noopener nofollow\">https:\/\/os.copernicus.org\/articles\/21\/2169\/2025\/os-21-2169-2025.html<\/a><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Autora de la not\u00edcia: <br><strong>Helena Fos<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><\/p>\n","protected":false},"featured_media":2658,"template":"","meta":{"_acf_changed":false,"inline_featured_image":false},"class_list":["post-2243","noticia","type-noticia","status-publish","has-post-thumbnail","hentry"],"acf":[],"_links":{"self":[{"href":"https:\/\/www.ub.edu\/geomarines\/web\/wp-json\/wp\/v2\/noticia\/2243","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.ub.edu\/geomarines\/web\/wp-json\/wp\/v2\/noticia"}],"about":[{"href":"https:\/\/www.ub.edu\/geomarines\/web\/wp-json\/wp\/v2\/types\/noticia"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.ub.edu\/geomarines\/web\/wp-json\/wp\/v2\/media\/2658"}],"wp:attachment":[{"href":"https:\/\/www.ub.edu\/geomarines\/web\/wp-json\/wp\/v2\/media?parent=2243"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}