{"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":"Influence of Anomalous Low-level Circulation on the Kuroshio in the Luzon Strait during ENSO - \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=\"jMu9ovvGsx\"><a href=\"https:\/\/www.oc.ntu.edu.tw\/en\/research-highlights\/16305\/\">Influence of Anomalous Low-level Circulation on the Kuroshio in the Luzon Strait during ENSO<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/www.oc.ntu.edu.tw\/en\/research-highlights\/16305\/embed\/#?secret=jMu9ovvGsx\" width=\"600\" height=\"338\" title=\"&#8220;Influence of Anomalous Low-level Circulation on the Kuroshio in the Luzon Strait during ENSO&#8221; &#8212; \u570b\u7acb\u81fa\u7063\u5927\u5b78\u6d77\u6d0b\u7814\u7a76\u6240 IO-NTU\" data-secret=\"jMu9ovvGsx\" 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","thumbnail_url":"https:\/\/www.oc.ntu.edu.tw\/wp-content\/uploads\/2023\/07\/FaceBook_iontu1.jpg","thumbnail_width":476,"thumbnail_height":246,"description":"The variation of Kuroshio loop in the Luzon Strait is important for the momentum, heat, and salt budgets of the SCS basin. Regarding the ENSO effects on the Kuroshio in the Luzon Strait, previous studies primarily focused on the effects of basin-scale wind anomalies and remote effects from the tropics. In this study, numerical experiments [&hellip;]"}