{"id":1001,"date":"2020-05-21T15:17:45","date_gmt":"2020-05-21T05:17:45","guid":{"rendered":"http:\/\/cosima.org.au\/?page_id=1001"},"modified":"2020-05-21T16:43:26","modified_gmt":"2020-05-21T06:43:26","slug":"session-3-model-applications","status":"publish","type":"page","link":"https:\/\/cosima.org.au\/index.php\/meetings\/cosima-v-workshop\/session-3-model-applications\/","title":{"rendered":"Session 3: Model applications"},"content":{"rendered":"<p><strong>Kial Stewart<\/strong>: Southern Ocean response to extreme SAM conditions<\/p>\n<iframe loading=\"lazy\"  id=\"_ytid_52016\"  width=\"821\" height=\"462\"  data-origwidth=\"821\" data-origheight=\"462\" src=\"https:\/\/www.youtube.com\/embed\/bHv6qnAQrrE?enablejsapi=1&autoplay=0&cc_load_policy=0&cc_lang_pref=&iv_load_policy=1&loop=0&modestbranding=0&rel=1&fs=1&playsinline=0&autohide=2&theme=dark&color=red&controls=1&\" class=\"__youtube_prefs__  no-lazyload\" title=\"YouTube player\"  allow=\"fullscreen; accelerometer; autoplay; clipboard-write; encrypted-media; gyroscope; picture-in-picture\" allowfullscreen data-no-lazy=\"1\" data-skipgform_ajax_framebjll=\"\"><\/iframe>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n<p><strong>Qian Li<\/strong>: Zonally asymmetric response of surface Southern Ocean to wind and thermal forcing<\/p>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n<p><strong>Matthew England<\/strong>: Role of wind variations in controlling ocean warming south of Australia<\/p>\n<iframe loading=\"lazy\"  id=\"_ytid_87194\"  width=\"821\" height=\"462\"  data-origwidth=\"821\" data-origheight=\"462\" src=\"https:\/\/www.youtube.com\/embed\/DsUMcmoAc6Q?enablejsapi=1&autoplay=0&cc_load_policy=0&cc_lang_pref=&iv_load_policy=1&loop=0&modestbranding=0&rel=1&fs=1&playsinline=0&autohide=2&theme=dark&color=red&controls=1&\" class=\"__youtube_prefs__  no-lazyload\" title=\"YouTube player\"  allow=\"fullscreen; accelerometer; autoplay; clipboard-write; encrypted-media; gyroscope; picture-in-picture\" allowfullscreen data-no-lazy=\"1\" data-skipgform_ajax_framebjll=\"\"><\/iframe>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n<p><strong>Veronica Tamsitt<\/strong>: Lagrangian pathways of Circumpolar Deep Water on the Antarctic continental shelf<\/p>\n<iframe loading=\"lazy\"  id=\"_ytid_74599\"  width=\"821\" height=\"462\"  data-origwidth=\"821\" data-origheight=\"462\" src=\"https:\/\/www.youtube.com\/embed\/5I0c027V-Jc?enablejsapi=1&autoplay=0&cc_load_policy=0&cc_lang_pref=&iv_load_policy=1&loop=0&modestbranding=0&rel=1&fs=1&playsinline=0&autohide=2&theme=dark&color=red&controls=1&\" class=\"__youtube_prefs__  no-lazyload\" title=\"YouTube player\"  allow=\"fullscreen; accelerometer; autoplay; clipboard-write; encrypted-media; gyroscope; picture-in-picture\" allowfullscreen data-no-lazy=\"1\" data-skipgform_ajax_framebjll=\"\"><\/iframe>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n<p><strong>Fabio Boeira Dias<\/strong>: Ocean heat storage driven by redistribution of heat in response to ocean circulation changes<\/p>\n<iframe loading=\"lazy\"  id=\"_ytid_27316\"  width=\"821\" height=\"462\"  data-origwidth=\"821\" data-origheight=\"462\" src=\"https:\/\/www.youtube.com\/embed\/Yw0lvtKWdhI?enablejsapi=1&autoplay=0&cc_load_policy=0&cc_lang_pref=&iv_load_policy=1&loop=0&modestbranding=0&rel=1&fs=1&playsinline=0&autohide=2&theme=dark&color=red&controls=1&\" class=\"__youtube_prefs__  no-lazyload\" title=\"YouTube player\"  allow=\"fullscreen; accelerometer; autoplay; clipboard-write; encrypted-media; gyroscope; picture-in-picture\" allowfullscreen data-no-lazy=\"1\" data-skipgform_ajax_framebjll=\"\"><\/iframe>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n<p><strong>Yi Jin<\/strong>: Regional ocean downscaling in Asian marginal seas<\/p>\n<iframe loading=\"lazy\"  id=\"_ytid_22210\"  width=\"821\" height=\"462\"  data-origwidth=\"821\" data-origheight=\"462\" src=\"https:\/\/www.youtube.com\/embed\/ryNjK6KQdiw?enablejsapi=1&autoplay=0&cc_load_policy=0&cc_lang_pref=&iv_load_policy=1&loop=0&modestbranding=0&rel=1&fs=1&playsinline=0&autohide=2&theme=dark&color=red&controls=1&\" class=\"__youtube_prefs__  no-lazyload\" title=\"YouTube player\"  allow=\"fullscreen; accelerometer; autoplay; clipboard-write; encrypted-media; gyroscope; picture-in-picture\" allowfullscreen data-no-lazy=\"1\" data-skipgform_ajax_framebjll=\"\"><\/iframe>\n","protected":false},"excerpt":{"rendered":"<p>Kial Stewart: Southern Ocean response to extreme SAM conditions &nbsp; &nbsp; Qian Li: Zonally asymmetric response of surface Southern Ocean to wind and thermal forcing &nbsp; &nbsp; Matthew England: Role of wind variations in controlling ocean warming south of Australia &nbsp; &nbsp; Veronica Tamsitt: Lagrangian pathways of Circumpolar Deep Water on the Antarctic continental shelf&hellip;<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":911,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"_links":{"self":[{"href":"https:\/\/cosima.org.au\/index.php\/wp-json\/wp\/v2\/pages\/1001"}],"collection":[{"href":"https:\/\/cosima.org.au\/index.php\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/cosima.org.au\/index.php\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/cosima.org.au\/index.php\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/cosima.org.au\/index.php\/wp-json\/wp\/v2\/comments?post=1001"}],"version-history":[{"count":3,"href":"https:\/\/cosima.org.au\/index.php\/wp-json\/wp\/v2\/pages\/1001\/revisions"}],"predecessor-version":[{"id":1005,"href":"https:\/\/cosima.org.au\/index.php\/wp-json\/wp\/v2\/pages\/1001\/revisions\/1005"}],"up":[{"embeddable":true,"href":"https:\/\/cosima.org.au\/index.php\/wp-json\/wp\/v2\/pages\/911"}],"wp:attachment":[{"href":"https:\/\/cosima.org.au\/index.php\/wp-json\/wp\/v2\/media?parent=1001"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}