{"version":"1.0","provider_name":"\u570b\u7acb\u81fa\u7063\u5927\u5b78\u6d77\u6d0b\u7814\u7a76\u6240 IO-NTU","provider_url":"https:\/\/www.oc.ntu.edu.tw\/en\/","title":"Impact of ENSO on the South China Sea during ENSO decaying periods (a new mesoscale perspective from the regional coupled model) - \u570b\u7acb\u81fa\u7063\u5927\u5b78\u6d77\u6d0b\u7814\u7a76\u6240 IO-NTU","type":"rich","width":600,"height":338,"html":"<blockquote class=\"wp-embedded-content\" data-secret=\"9tuXyWhCxP\"><a href=\"https:\/\/www.oc.ntu.edu.tw\/en\/research-highlights\/15994\/\">Impact of ENSO on the South China Sea during ENSO decaying periods (a new mesoscale perspective from the regional coupled model)<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/www.oc.ntu.edu.tw\/en\/research-highlights\/15994\/embed\/#?secret=9tuXyWhCxP\" width=\"600\" height=\"338\" title=\"&#8220;Impact of ENSO on the South China Sea during ENSO decaying periods (a new mesoscale perspective from the regional coupled model)&#8221; &#8212; \u570b\u7acb\u81fa\u7063\u5927\u5b78\u6d77\u6d0b\u7814\u7a76\u6240 IO-NTU\" data-secret=\"9tuXyWhCxP\" frameborder=\"0\" marginwidth=\"0\" marginheight=\"0\" scrolling=\"no\" class=\"wp-embedded-content\"><\/iframe><script>\n\/*! This file is auto-generated *\/\n!function(d,l){\"use strict\";l.querySelector&&d.addEventListener&&\"undefined\"!=typeof URL&&(d.wp=d.wp||{},d.wp.receiveEmbedMessage||(d.wp.receiveEmbedMessage=function(e){var t=e.data;if((t||t.secret||t.message||t.value)&&!\/[^a-zA-Z0-9]\/.test(t.secret)){for(var s,r,n,a=l.querySelectorAll('iframe[data-secret=\"'+t.secret+'\"]'),o=l.querySelectorAll('blockquote[data-secret=\"'+t.secret+'\"]'),c=new RegExp(\"^https?:$\",\"i\"),i=0;i<o.length;i++)o[i].style.display=\"none\";for(i=0;i<a.length;i++)s=a[i],e.source===s.contentWindow&&(s.removeAttribute(\"style\"),\"height\"===t.message?(1e3<(r=parseInt(t.value,10))?r=1e3:~~r<200&&(r=200),s.height=r):\"link\"===t.message&&(r=new URL(s.getAttribute(\"src\")),n=new URL(t.value),c.test(n.protocol))&&n.host===r.host&&l.activeElement===s&&(d.top.location.href=t.value))}},d.addEventListener(\"message\",d.wp.receiveEmbedMessage,!1),l.addEventListener(\"DOMContentLoaded\",function(){for(var e,t,s=l.querySelectorAll(\"iframe.wp-embedded-content\"),r=0;r<s.length;r++)(t=(e=s[r]).getAttribute(\"data-secret\"))||(t=Math.random().toString(36).substring(2,12),e.src+=\"#?secret=\"+t,e.setAttribute(\"data-secret\",t)),e.contentWindow.postMessage({message:\"ready\",secret:t},\"*\")},!1)))}(window,document);\n<\/script>\n","description":"The South China Sea (SCS) is the largest marginal sea in the western North Pacific. Its surface thermal conditions greatly affect the weather and climate conditions in the sea and its adjacent landmass. Previous studies have suggested that the ocean dynamics in the SCS play a crucial role in local air\u2013sea processes so as to [&hellip;]","thumbnail_url":"https:\/\/www.oc.ntu.edu.tw\/wp-content\/uploads\/2020\/08\/image001.png"}