{"id":469,"date":"2022-11-26T10:54:28","date_gmt":"2022-11-26T02:54:28","guid":{"rendered":"http:\/\/www.fvcom.org\/?p=469"},"modified":"2022-12-16T14:28:48","modified_gmt":"2022-12-16T06:28:48","slug":"satilla","status":"publish","type":"post","link":"https:\/\/www.fvcom.org\/?p=469","title":{"rendered":"The Satilla"},"content":{"rendered":"\n<p class=\"has-text-align-center has-medium-font-size wp-block-paragraph\">Block 1<\/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=\"575\" style=\"aspect-ratio: 695 \/ 575;\" width=\"695\" controls poster=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/82.jpg\" src=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/1_FVCOM_satilla_river_currents.mov\"><\/video><figcaption class=\"wp-element-caption\">The animation displays the tidal current variability over an M<sub>2 <\/sub>tidal cycle in the Satilla River, Georgia, U.S.A<\/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=\"600\" style=\"aspect-ratio: 700 \/ 600;\" width=\"700\" controls poster=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/83.jpg\" src=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/2_FVCOM_satilla_river_NH4.mov\"><\/video><figcaption class=\"wp-element-caption\">The animation displays the variability of the NH<sub>4<\/sub> concentration over an M<sub>2 <\/sub>tidal cycle in the Satilla River, Georgia, U.S.A.<\/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=\"600\" style=\"aspect-ratio: 700 \/ 600;\" width=\"700\" controls poster=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/84.jpg\" src=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/3_FVCOM_satilla_river_chla.mov\"><\/video><figcaption class=\"wp-element-caption\">1.&nbsp;&nbsp;&nbsp;&nbsp; The animation displays the variability of the Chl-a concentration over an M<sub>2 <\/sub>tidal cycle in the Satilla River, Georgia, U.S.A.<\/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=\"600\" style=\"aspect-ratio: 700 \/ 600;\" width=\"700\" controls poster=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/85.jpg\" src=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/4_FVCOM_satilla_river_DO.mov\"><\/video><figcaption class=\"wp-element-caption\">1.&nbsp;&nbsp;&nbsp;&nbsp; The animation displays the variability of the DO concentration over an M<sub>2 <\/sub>tidal cycle in the Satilla River, Georgia, U.S.A.<\/figcaption><\/figure>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\"><\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\"><\/div>\n<\/div>\n\n\n\n<p class=\"wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"has-text-align-center has-medium-font-size wp-block-paragraph\">Block 2<\/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=\"575\" style=\"aspect-ratio: 658 \/ 575;\" width=\"658\" controls poster=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/86.jpg\" src=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/5_FVCOM_satilla_river_particles_HW.mov\"><\/video><figcaption class=\"wp-element-caption\">The animation displays the trajectories of particles released at high tide in the Satilla River, Georgia, the U.S.A., 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=\"575\" style=\"aspect-ratio: 658 \/ 575;\" width=\"658\" controls poster=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/87.jpg\" src=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/6_FVCOM_satilla_river_particles_LW.mov\"><\/video><figcaption class=\"wp-element-caption\">The animation displays the trajectories of particles released at low tide in the Satilla River, Georgia, U.S.A., 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=\"583\" style=\"aspect-ratio: 658 \/ 583;\" width=\"658\" controls poster=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/88.jpg\" src=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/7_FVCOM_satilla_river_particles_HW_wind.mov\"><\/video><figcaption class=\"wp-element-caption\">The animation displays the trajectories of particles released at high tide in the Satilla River, Georgia, U.S.A., under tidal and wind forcing conditions.<\/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=\"575\" style=\"aspect-ratio: 658 \/ 575;\" width=\"658\" controls poster=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/89.jpg\" src=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/8_FVCOM_satilla_river-particles_LW_wind.mov\"><\/video><figcaption class=\"wp-element-caption\">The animation displays the trajectories of particles released at low tide in the Satilla River, Georgia, U.S.A., under tidal and wind forcing conditions.<\/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=\"505\" style=\"aspect-ratio: 811 \/ 505;\" width=\"811\" controls poster=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/90.jpg\" src=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/9_FVCOM_ECO-si_satilla_river_low_particle_anim.mov\"><\/video><figcaption class=\"wp-element-caption\">The animation compared the FVCOM and ECOM-si-predicted trajectories of particles released over the salt march at low tide in the Satilla River, Georgia, U.S.A. The only tidal forcing was considered.<\/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=\"438\" style=\"aspect-ratio: 811 \/ 438;\" width=\"811\" controls poster=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/91.jpg\" src=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/10_FVCOM_ECOM-SI_comp_high_particle_anim.mov\"><\/video><figcaption class=\"wp-element-caption\">The animation compared the FVCOM and ECOM-si-predicted trajectories of particles released over the salt march at high tide in the Satilla River, Georgia, U.S.A. The only tidal forcing was considered.<\/figcaption><\/figure>\n<\/div>\n<\/div>\n\n\n\n<p class=\"has-text-align-center has-medium-font-size wp-block-paragraph\">Block 3<\/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=\"480\" style=\"aspect-ratio: 640 \/ 480;\" width=\"640\" controls poster=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/92.jpg\" src=\"https:\/\/www.fvcom.org\/wp-content\/uploads\/2022\/11\/11_Satilla_suspen.mov\"><\/video><figcaption class=\"wp-element-caption\">The animation displays the variability of suspended sediment concentration (SSC) along the Satilla River, Georgia, U.S.A. The only tidal forcing was considered.<\/figcaption><\/figure>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\"><\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\"><\/div>\n<\/div>\n","protected":false},"excerpt":{"rendered":"<p>Block 1 Block 2 Block 3<\/p>\n","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-469","post","type-post","status-publish","format-standard","hentry","category-research"],"_links":{"self":[{"href":"https:\/\/www.fvcom.org\/index.php?rest_route=\/wp\/v2\/posts\/469","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=469"}],"version-history":[{"count":9,"href":"https:\/\/www.fvcom.org\/index.php?rest_route=\/wp\/v2\/posts\/469\/revisions"}],"predecessor-version":[{"id":1516,"href":"https:\/\/www.fvcom.org\/index.php?rest_route=\/wp\/v2\/posts\/469\/revisions\/1516"}],"wp:attachment":[{"href":"https:\/\/www.fvcom.org\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=469"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.fvcom.org\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=469"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.fvcom.org\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=469"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}