{"id":174,"date":"2010-04-09T08:23:00","date_gmt":"2010-04-09T08:23:00","guid":{"rendered":"http:\/\/blogs.agu.org\/landslideblog\/2010\/04\/09\/latest-update-on-the-attabad-landslide\/"},"modified":"2010-10-21T13:35:54","modified_gmt":"2010-10-21T17:35:54","slug":"latest-update-on-the-attabad-landslide","status":"publish","type":"post","link":"https:\/\/blogs.agu.org\/landslideblog\/2010\/04\/09\/latest-update-on-the-attabad-landslide\/","title":{"rendered":"Latest Update on the Attabad landslide"},"content":{"rendered":"<p>Whilst my <a href=\"http:\/\/hunzalandslide.blogspot.com\/\">Hunza Landslide Monitoring website<\/a> is the main location for the monitoring data of the <a href=\"https:\/\/blogs.agu.org\/wp-content\/scripts\/daveslandslideblog.blogspot.com.bouncer.php\/daveslandslideblog.blogspot.com\/2010\/04\/new-images-of-attabad-landslide.html\">landslide at Attabad<\/a>, I will continue to put updates here every few days.&nbsp; The current situation is that the lake level continues to rise at 30 to 40 cm per day.&nbsp; This is perhaps slightly lower than expected as temperatures in this region remain unseasonably cold, meaning that snowmelt (and thus inflow) has been delayed.&nbsp; Based upon the current rate of rise of the lake level and downcutting of the channel, the water should reach the spillway in two to three months.&nbsp; This may shorten if the rate of inflow increases.<\/p>\n<p>This graph shows the water level through time and the level of the spillway, based upon NDMA and Focus data:<\/p>\n<div class=\"separator\" style=\"clear: both;text-align: center\"><\/div>\n<div class=\"separator\" style=\"clear: both;text-align: center\"><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/10_04-Hunza-lake-level-4.jpg\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"251\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/10_04-Hunza-lake-level-4.jpg\" width=\"400\" \/><\/a><\/div>\n<p>Meanwhile, this one shows the rate of seepage at the three points plus the overall rate.&nbsp; It is clear that the seepage rate has stabilised over the last few days:<\/p>\n<div class=\"separator\" style=\"clear: both;text-align: center\"><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/10_04-Hunza-seepage-4.jpg\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"251\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/10_04-Hunza-seepage-4.jpg\" width=\"400\" \/><\/a><\/div>\n<!-- AddThis Advanced Settings generic via filter on the_content --><!-- AddThis Share Buttons generic via filter on the_content -->","protected":false},"excerpt":{"rendered":"<p>Whilst my Hunza Landslide Monitoring website is the main location for the monitoring data of the landslide at Attabad, I will continue to put updates here every few days.&nbsp; The current situation is that the lake level continues to rise at 30 to 40 cm per day.&nbsp; This is perhaps slightly lower than expected as temperatures in this region remain unseasonably cold, meaning that snowmelt (and thus inflow) has been &hellip;<!-- AddThis Advanced Settings generic via filter on wp_trim_excerpt --><!-- AddThis Share Buttons generic via filter on wp_trim_excerpt --><\/p>\n","protected":false},"author":22,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[],"class_list":["post-174","post","type-post","status-publish","format-standard","hentry","category-uncategorized"],"_links":{"self":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/174","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/users\/22"}],"replies":[{"embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/comments?post=174"}],"version-history":[{"count":0,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/174\/revisions"}],"wp:attachment":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media?parent=174"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/categories?post=174"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/tags?post=174"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}