{"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":"Seasonal Changes in Gaseous Elemental Mercury in Relation to Monsoon Cycling over the Northern South China Sea - \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=\"d4SOa3qlj5\"><a href=\"https:\/\/www.oc.ntu.edu.tw\/en\/news-en\/28386\/\">Seasonal Changes in Gaseous Elemental Mercury in Relation to Monsoon Cycling over the Northern South China Sea<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/www.oc.ntu.edu.tw\/en\/news-en\/28386\/embed\/#?secret=d4SOa3qlj5\" width=\"600\" height=\"338\" title=\"&#8220;Seasonal Changes in Gaseous Elemental Mercury in Relation to Monsoon Cycling over the Northern South China Sea&#8221; &#8212; \u570b\u7acb\u81fa\u7063\u5927\u5b78\u6d77\u6d0b\u7814\u7a76\u6240 IO-NTU\" data-secret=\"d4SOa3qlj5\" 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":"Seasonal Changes in Gaseous Elemental Mercury in Relation to Monsoon Cycling over the Northern South China Sea Tseng, C. M., Liu, C. S., Lamborg, C., (2012), Atmos. Chem. Phys., 12, 7341-7350, doi:10.5194\/acp-12-7341-2012. www.atmos-chem-phys.net\/12\/7341\/2012\/ The distribution of gaseous elemental mercury (GEM) was determined in the surface atmosphere of the northern South China Sea (SCS) during 12 [&hellip;]","thumbnail_url":"https:\/\/www.oc.ntu.edu.tw\/wp-content\/uploads\/2012\/10\/research_Tseng.png"}