{"id":597,"date":"2022-11-26T12:50:52","date_gmt":"2022-11-26T04:50:52","guid":{"rendered":"http:\/\/www.fvcom.org\/?p=597"},"modified":"2022-12-16T11:07:27","modified_gmt":"2022-12-16T03:07:27","slug":"nantucket-sound","status":"publish","type":"post","link":"https:\/\/www.fvcom.org\/?p=597","title":{"rendered":"Nantucket Sound"},"content":{"rendered":"\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-8f761849 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<figure class=\"wp-block-video\"><video height=\"540\" style=\"aspect-ratio: 656 \/ 540;\" width=\"656\" controls poster=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/61.jpg\" src=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/1_FVCOM_NS_tidal_currents.mov\"><\/video><figcaption class=\"wp-element-caption\">The animation displays the M<sub>2<\/sub> tidal flow change in Nantucket Sound. The simulation was done using FVCOM with a horizontal resolution of up to ~100 m.<\/figcaption><\/figure>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<figure class=\"wp-block-video\"><video height=\"640\" style=\"aspect-ratio: 740 \/ 640;\" width=\"740\" controls poster=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/62.jpg\" src=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/2_FVCOM_NS_199904_residual_flow.mov\"><\/video><figcaption class=\"wp-element-caption\">The animation displayed the variability of the surface temperature and subtidal currents in Nantucket Sound in April 1999. The simulation was done using FVCOM with a horizontal resolution of up to ~100 m.<\/figcaption><\/figure>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<figure class=\"wp-block-video\"><video height=\"640\" style=\"aspect-ratio: 740 \/ 640;\" width=\"740\" controls poster=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/63.jpg\" src=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/3_FVCOM_NS_199908_residual_flow-1.mov\"><\/video><figcaption class=\"wp-element-caption\">The animation displayed the variability of the surface temperature and subtidal currents in Nantucket Sound in August 1999. The simulation was done using FVCOM with a horizontal resolution of up to ~100 m.<\/figcaption><\/figure>\n<\/div>\n<\/div>\n","protected":false},"excerpt":{"rendered":"","protected":false},"author":1,"featured_media":0,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[12],"tags":[],"class_list":["post-597","post","type-post","status-publish","format-standard","hentry","category-research"],"_links":{"self":[{"href":"https:\/\/www.fvcom.org\/index.php?rest_route=\/wp\/v2\/posts\/597","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.fvcom.org\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.fvcom.org\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.fvcom.org\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.fvcom.org\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=597"}],"version-history":[{"count":3,"href":"https:\/\/www.fvcom.org\/index.php?rest_route=\/wp\/v2\/posts\/597\/revisions"}],"predecessor-version":[{"id":1372,"href":"https:\/\/www.fvcom.org\/index.php?rest_route=\/wp\/v2\/posts\/597\/revisions\/1372"}],"wp:attachment":[{"href":"https:\/\/www.fvcom.org\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=597"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.fvcom.org\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=597"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.fvcom.org\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=597"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}