{"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":"Oceanic Whispering Gallery Effect Between Shelfbreak and Internal Waves - \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=\"LdgpSB9QEA\"><a href=\"https:\/\/www.oc.ntu.edu.tw\/en\/research-highlights\/35591\/\">Oceanic Whispering Gallery Effect Between Shelfbreak and Internal Waves<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/www.oc.ntu.edu.tw\/en\/research-highlights\/35591\/embed\/#?secret=LdgpSB9QEA\" width=\"600\" height=\"338\" title=\"&#8220;Oceanic Whispering Gallery Effect Between Shelfbreak and Internal Waves&#8221; &#8212; \u570b\u7acb\u81fa\u7063\u5927\u5b78\u6d77\u6d0b\u7814\u7a76\u6240 IO-NTU\" data-secret=\"LdgpSB9QEA\" 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\/2025\/02\/NIWs.jpg","thumbnail_width":966,"thumbnail_height":645,"description":"Nonlinear Internal Gravity Waves (NIWs) significantly influence sound propagation in the ocean, particularly in shelfbreak areas. Variations in water depth and vertical stratification complicate acoustic transmission. To investigate these effects, Assistant Professor Tzu-Ting Chen and her research team integrated experimental data and simulations across multiple disciplines, including marine geology and geophysics (high-resolution bathymetry), underwater acoustics, [&hellip;]"}