{"version":"1.0","provider_name":"Departemen Teknik Geofisika","provider_url":"https:\/\/www.its.ac.id\/tgeofisika","author_name":"Admin-Teknik Geofisika","author_url":"https:\/\/www.its.ac.id\/tgeofisika\/author\/tgeofisikaadmin\/","title":"WEBINAR#66 \"ANTISIPASI EL NINO DAN KEKERINGAN\" - Departemen Teknik Geofisika","type":"rich","width":600,"height":338,"html":"<blockquote class=\"wp-embedded-content\" data-secret=\"aiRbdf2JfC\"><a href=\"https:\/\/www.its.ac.id\/tgeofisika\/webinar66-antisipasi-el-nino-dan-kekeringan-2\/\">WEBINAR#66 &#8220;ANTISIPASI EL NINO DAN KEKERINGAN&#8221;<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/www.its.ac.id\/tgeofisika\/webinar66-antisipasi-el-nino-dan-kekeringan-2\/embed\/#?secret=aiRbdf2JfC\" width=\"600\" height=\"338\" title=\"&#8220;WEBINAR#66 &#8220;ANTISIPASI EL NINO DAN KEKERINGAN&#8221;&#8221; &#8212; Departemen Teknik Geofisika\" data-secret=\"aiRbdf2JfC\" 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\/\/# sourceURL=https:\/\/www.its.ac.id\/tgeofisika\/wp-includes\/js\/wp-embed.min.js\n<\/script>\n","thumbnail_url":"https:\/\/www.its.ac.id\/tgeofisika\/wp-content\/uploads\/sites\/33\/2023\/05\/Webinar-Antisipasi-Elnino-dan-Kekeringan-oleh-Teknik-Geofisika-ITS.png","thumbnail_width":1080,"thumbnail_height":1080,"description":"LATAR BELAKANG El Nino adalah fenomena pemanasan Suhu Muka Laut (SML) di atas kondisi normalnya yang terjadi di Samudera Pasifik bagian tengah. Pemanasan SML ini meningkatkan potensi pertumbuhan awan di Samudera Pasifik tengah dan mengurangi curah hujan di wilayah Indonesia. Singkatnya, El Nino memicu terjadinya kondisi kekeringan untuk wilayah Indonesia secara umum. Sebaliknya La Nina [&hellip;]"}