{"version":"1.0","provider_name":"PermafrostNet","provider_url":"https:\/\/permafrostnet.ca\/fr","author_name":"nick brown","author_url":"https:\/\/permafrostnet.ca\/fr\/author\/nickbrown\/","title":"PhD in thaw pond initiation and evolution pathways &#8211; PermafrostNet","type":"rich","width":600,"height":338,"html":"<blockquote class=\"wp-embedded-content\" data-secret=\"WyeYKYBLpN\"><a href=\"https:\/\/permafrostnet.ca\/fr\/opportunity\/grad\/phd-thaw-pond-init-evo\/\">PhD in thaw pond initiation and evolution pathways<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/permafrostnet.ca\/fr\/opportunity\/grad\/phd-thaw-pond-init-evo\/embed\/#?secret=WyeYKYBLpN\" width=\"600\" height=\"338\" title=\"&laquo; PhD in thaw pond initiation and evolution pathways &raquo; &#8212; PermafrostNet\" data-secret=\"WyeYKYBLpN\" frameborder=\"0\" marginwidth=\"0\" marginheight=\"0\" scrolling=\"no\" class=\"wp-embedded-content\"><\/iframe><script type=\"text\/javascript\">\n\/* <![CDATA[ *\/\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:\/\/permafrostnet.ca\/wp-includes\/js\/wp-embed.min.js\n\/* ]]> *\/\n<\/script>","description":"This position will elucidate controls on 1) the initiation of thaw lakes and ponds, 2) variation in rates of expansion, and 3) pathways of stabilization and permafrost recovery post stabilization. Field work will take place in thermokarst-affected lowlands between the Blackstone Uplands (YT) and Tuktoyuktuk (NWT). The position will develop predictive models based on the interacting effects of paleogeography (deposits and ice), climate, topography, snow cover, and vegetation growth within thaw ponds.","thumbnail_url":"https:\/\/permafrostnet.ca\/wp-content\/uploads\/2019\/10\/Dempster-road-lighter.jpg","thumbnail_width":1920,"thumbnail_height":1275}