The central Mozambique Channel and its coastal communities is our study area<\/strong>. The three figures are based on a daily average (December 1st, 2014) of a high-resolution (1\/36\u00b0) ROMS-CROCO configuration (P. Penven).<\/p>- a. Sea Surface Temperature (SST, in \u00b0C) showing a southward flow of warm tropical waters across the Mozambique Channel.<\/li>
- b. Surface vorticity (vorticity\/f): blues and reds represent high energy areas related to ocean fronts and eddies.<\/li>
- c. Ocean fronts (SST gradients, \u00b0C\/km, Belkin and O'Reilly): strong fronts, potentially forming ephemeral ecosystems, are highlighted in bright white and red.<\/li><\/ul><\/td><\/tr><\/tbody><\/table> <\/div> <\/div><\/section><\/div><\/div><\/div><\/div> <\/div> <\/div> <\/div> <\/div><\/div>","protected":false},"featured_media":4489,"parent":0,"template":"","class_list":["post-7291","archive_page","type-archive_page","status-publish","has-post-thumbnail","hentry"],"acf":{"id_old":"3081","category_old":"Mers et oc\u00e9ans Changement global"},"_links":{"self":[{"href":"https:\/\/www.mio.osupytheas.fr\/en\/wp-json\/wp\/v2\/archive_page\/7291","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.mio.osupytheas.fr\/en\/wp-json\/wp\/v2\/archive_page"}],"about":[{"href":"https:\/\/www.mio.osupytheas.fr\/en\/wp-json\/wp\/v2\/types\/archive_page"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.mio.osupytheas.fr\/en\/wp-json\/wp\/v2\/media\/4489"}],"wp:attachment":[{"href":"https:\/\/www.mio.osupytheas.fr\/en\/wp-json\/wp\/v2\/media?parent=7291"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}
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