{"id":552,"date":"2022-11-26T12:17:06","date_gmt":"2022-11-26T04:17:06","guid":{"rendered":"http:\/\/www.fvcom.org\/?p=552"},"modified":"2022-12-16T13:12:24","modified_gmt":"2022-12-16T05:12:24","slug":"the-east-china-sea","status":"publish","type":"post","link":"https:\/\/www.fvcom.org\/?p=552","title":{"rendered":"The East China Sea"},"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=\"480\" style=\"aspect-ratio: 720 \/ 480;\" width=\"720\" controls poster=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/124.jpg\" src=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/1_ecscj-2.mov\"><\/video><figcaption class=\"wp-element-caption\">The animation displays the FVCOM-simulated near-surface M<sub>2<\/sub>-tidal currents and elevation in the East China Sea.<\/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=\"715\" style=\"aspect-ratio: 700 \/ 715;\" width=\"700\" controls poster=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/125.jpg\" src=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/2_kuroshio-2.mov\"><\/video><figcaption class=\"wp-element-caption\">The animation displays the FVCOM-predicted near-surface temperature and currents in the East China Sea. &nbsp;The simulation was done through a nesting with Global-FVCOM.<\/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=\"740\" style=\"aspect-ratio: 700 \/ 740;\" width=\"700\" controls poster=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/126.jpg\" src=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/3_FVCOM_ecs_salt_curr_wind.mov\"><\/video><figcaption class=\"wp-element-caption\">The animation displays the development of the FVCOM-predicted low-salinity plume in the inner shelf connecting to the Changjiang Estuary in the East China Sea.<\/figcaption><\/figure>\n<\/div>\n<\/div>\n\n\n\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=\"846\" style=\"aspect-ratio: 750 \/ 846;\" width=\"750\" controls poster=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/127.jpg\" src=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/4_ECS_wrf_WindPressure.mov\"><\/video><figcaption class=\"wp-element-caption\">The animation shows an example of the WRF-predicted sea-surface pressure and winds over the East China Sea.<\/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=\"700\" style=\"aspect-ratio: 600 \/ 700;\" width=\"600\" controls poster=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/128.jpg\" src=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/5_FVCOM_ECS_particles_nowind.mov\"><\/video><figcaption class=\"wp-element-caption\">The animation displays the trajectories of particles released near the surface (upper) and bottom (lower) within the Changjiang Estuary under a condition with only tidal forcing.<\/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=\"700\" style=\"aspect-ratio: 600 \/ 700;\" width=\"600\" controls poster=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/129.jpg\" src=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/6_FVCOM_ECS_particles_wind.mov\"><\/video><figcaption class=\"wp-element-caption\">The animation displays the trajectories of particles released near the surface (upper) and bottom (lower) within the Changjiang Estuary under conditions with only tidal and wind forcings.<\/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-552","post","type-post","status-publish","format-standard","hentry","category-research"],"_links":{"self":[{"href":"https:\/\/www.fvcom.org\/index.php?rest_route=\/wp\/v2\/posts\/552","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=552"}],"version-history":[{"count":6,"href":"https:\/\/www.fvcom.org\/index.php?rest_route=\/wp\/v2\/posts\/552\/revisions"}],"predecessor-version":[{"id":1461,"href":"https:\/\/www.fvcom.org\/index.php?rest_route=\/wp\/v2\/posts\/552\/revisions\/1461"}],"wp:attachment":[{"href":"https:\/\/www.fvcom.org\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=552"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.fvcom.org\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=552"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.fvcom.org\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=552"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}