{"id":521,"date":"2022-11-26T11:42:15","date_gmt":"2022-11-26T03:42:15","guid":{"rendered":"http:\/\/www.fvcom.org\/?p=521"},"modified":"2022-12-16T13:04:16","modified_gmt":"2022-12-16T05:04:16","slug":"the-changjiang-river","status":"publish","type":"post","link":"https:\/\/www.fvcom.org\/?p=521","title":{"rendered":"The Changjiang River"},"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=\"610\" style=\"aspect-ratio: 784 \/ 610;\" width=\"784\" controls poster=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/116.jpg\" src=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/1_FVCOM_CJ_tidal_currents.mp4\"><\/video><figcaption class=\"wp-element-caption\">The animation displays the FVCOM-simulated near-surface M<sub>2<\/sub>-tidal currents in the Changjiang Estuary.<\/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=\"400\" style=\"aspect-ratio: 636 \/ 400;\" width=\"636\" controls poster=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/117.jpg\" src=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/2_FVCOM_CJ_dikes_tidal_currents.mov\"><\/video><figcaption class=\"wp-element-caption\">The animation displays the FVCOM-predicted near-surface currents around the navigation channel with dikes and groynes off the Changjiang River. The simulation did not include FVCOM dike-groyne module.<\/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=\"801\" style=\"aspect-ratio: 860 \/ 801;\" width=\"860\" controls poster=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/118.jpg\" src=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/3_FVCOM_dam_surface.mov\"><\/video><figcaption class=\"wp-element-caption\">The animation displays the FVCOM-predicted near-surface currents around the navigation channel with dikes and groynes off the Changjiang River. The simulation included the FVCOM dike-groyne module.<\/figcaption><\/figure>\n<\/div>\n<\/div>\n\n\n\n<p class=\"wp-block-paragraph\"><\/p>\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=\"801\" style=\"aspect-ratio: 860 \/ 801;\" width=\"860\" controls poster=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/119.jpg\" src=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/4_FVCOM_dam_bottom.mov\"><\/video><figcaption class=\"wp-element-caption\">The animation displays the FVCOM-predicted near-bottom currents around the navigation channel with dikes and groynes off the Changjiang River. The simulation included the FVCOM dike-groyne module.<\/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=\"578\" style=\"aspect-ratio: 824 \/ 578;\" width=\"824\" controls poster=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/120.jpg\" src=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/5_FVCOM_CJ_runoff_summer-1.mov\"><\/video><figcaption class=\"wp-element-caption\">The animation displays the evolution process of the Changjiang River\u2019s low-salinity plume due to the freshwater discharge from the upstream area.<\/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=\"580\" style=\"aspect-ratio: 921 \/ 580;\" width=\"921\" controls poster=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/121.jpg\" src=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/6_FVCOM_CJ_runoff_winter.mov\"><\/video><figcaption class=\"wp-element-caption\">The animation displays the saltwater intrusion enhanced by the wind within the Changjiang River<\/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-521","post","type-post","status-publish","format-standard","hentry","category-research"],"_links":{"self":[{"href":"https:\/\/www.fvcom.org\/index.php?rest_route=\/wp\/v2\/posts\/521","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=521"}],"version-history":[{"count":8,"href":"https:\/\/www.fvcom.org\/index.php?rest_route=\/wp\/v2\/posts\/521\/revisions"}],"predecessor-version":[{"id":1450,"href":"https:\/\/www.fvcom.org\/index.php?rest_route=\/wp\/v2\/posts\/521\/revisions\/1450"}],"wp:attachment":[{"href":"https:\/\/www.fvcom.org\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=521"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.fvcom.org\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=521"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.fvcom.org\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=521"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}