{"id":35,"date":"2010-08-13T08:31:00","date_gmt":"2010-08-13T08:31:00","guid":{"rendered":"http:\/\/blogs.agu.org\/landslideblog\/2010\/08\/13\/update-on-china-and-pakistan-13th-august-2010\/"},"modified":"2010-10-21T13:35:08","modified_gmt":"2010-10-21T17:35:08","slug":"update-on-china-and-pakistan-13th-august-2010","status":"publish","type":"post","link":"https:\/\/blogs.agu.org\/landslideblog\/2010\/08\/13\/update-on-china-and-pakistan-13th-august-2010\/","title":{"rendered":"Update on China and Pakistan &#8211; 13th August 2010"},"content":{"rendered":"<p><b>1. The Gansu landslide in China<\/b><br \/>The rescue operations in Gansu have now clearly transitioned into a recovery and rehabilitation phase, greatly hampered by continuing very heavy rainfall in the area.&nbsp; <a href=\"http:\/\/news.xinhuanet.com\/english2010\/china\/2010-08\/13\/c_13443406.htm\">Landslides are continuing to occur<\/a> in the area, with resultant casualties.<\/p>\n<p><a href=\"http:\/\/lboro.ac.uk\/departments\/cv\/staff\/profile\/166.html\">Tom Dijkstra of Loughborough University<\/a> visited the site as part of a trip to look at collaborative landslide research in the area back in November.&nbsp; He has kindly sent two images of the town to me and has agreed that I can put them online.&nbsp; This image shows the area affected by the landslide from the other side of the river.&nbsp; The steep, deforested mountains in the background are clearly the source of the flow:<\/p>\n<div class=\"separator\" style=\"clear: both;text-align: center\"><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/10_08-Gansu-15.jpg\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"428\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/10_08-Gansu-15.jpg\" width=\"640\" \/><\/a><\/div>\n<p>The second image shows the catchment source of the flow:<\/p>\n<div class=\"separator\" style=\"clear: both;text-align: center\"><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/10_08-Gansu-16.jpg\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"548\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/10_08-Gansu-16.jpg\" width=\"640\" \/><\/a><\/div>\n<p>It is worth comparing the above image with this <a href=\"http:\/\/uk.news.yahoo.com\/19\/20100809\/img\/pwl-china-floods-9556106-01170496304c.html\">AP picture<\/a> that <a href=\"https:\/\/blogs.agu.org\/wp-content\/scripts\/daveslandslideblog.blogspot.com.bouncer.php\/daveslandslideblog.blogspot.com\/2010\/08\/updates-for-pakistan-china-and-india.html\">I posted a few days<\/a> ago of the site after the flow:<\/p>\n<div class=\"separator\" style=\"clear: both;text-align: center\"><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/10_08-Gansu-17.jpg\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"265\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/10_08-Gansu-17.jpg\" width=\"400\" \/><\/a><\/div>\n<p>The reasons for the very high loss of life, now estimated to be 1,144 people, with a further 600 still missing, are clear given the density of buildings in the affected area.<\/p>\n<p><b>2. Pakistan<\/b><br \/>The two flood waves in Pakistan continue to cause extreme levels of suffering.&nbsp; According to the <a href=\"http:\/\/www.pakmet.com.pk\/FFD\/index_files\/hydro.htm\">FFD hydrographs<\/a> the water level at Sukkur is now falling slowly after the passage of the first flood wave:<\/p>\n<div class=\"separator\" style=\"clear: both;text-align: center\"><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/10_08-sukkur-10.gif\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"347\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/10_08-sukkur-10.gif\" width=\"640\" \/><\/a><\/div>\n<p>What has been particularly interesting though is that the flood level is not really increasing substantially at Kotri, the large gauging station downstream:<\/p>\n<div class=\"separator\" style=\"clear: both;text-align: center\"><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/10_08-kotri-10.gif\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"348\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/10_08-kotri-10.gif\" width=\"640\" \/><\/a><\/div>\n<p>This presumably means one of two things.&nbsp; First, it could be that the water is finding another route &#8211; i.e. that it is bypassing the gauging station.&nbsp; Alternatively, the water is in effect trapped between the two sites, which might explain the very slow falling limb of the hydrograph.&nbsp; The Google Earth satellite image below shows Kotri: <\/p>\n<div class=\"separator\" style=\"clear: both;text-align: center\"><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/10_08-Kotri-image.jpg\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"438\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/10_08-Kotri-image.jpg\" width=\"640\" \/><\/a><\/div>\n<p>It is possible that the water has flooded the adjacent land, but the <a href=\"http:\/\/www.reliefweb.int\/rw\/rwb.nsf\/db900SID\/NROI-88A6UP?OpenDocument\">news reports<\/a> indicate that this is not the case, with the suggestion that the bridges downstream of Sukkur are slowing the flow down.&nbsp; This is dangerous in the context of the second flood wave, which at the moment remains smaller than the first.&nbsp; This is the hydrograph for Taunsa, which is just below the &#8220;Extremely High&#8221; flood level:<\/p>\n<div class=\"separator\" style=\"clear: both;text-align: center\"><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/10_08-taunsa-10.gif\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"348\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/10_08-taunsa-10.gif\" width=\"640\" \/><\/a><\/div>\n<p>At Guddu the discharge is still falling, but only very slowly.&nbsp; Indeed the discharge remains well above the &#8220;Exceptionally High&#8221; level:<\/p>\n<div class=\"separator\" style=\"clear: both;text-align: center\"><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/10_08-guddu-10.gif\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"347\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/10_08-guddu-10.gif\" width=\"640\" \/><\/a><\/div>\n<p>The danger must be that the second flood wave starts to catch up with, and build upon, the stalled first wave.&nbsp; This would create the potential for an extremely damaging second phase of floods.&nbsp; It took six days for the first wave to pass from Taunsa to Guddu, and a further day to Sukkur.&nbsp; The hope must be that the water level starts to fall quickly at these two sites before the second wave arrives.<\/p>\n<p>Unfortunately, it is clear that this slow motion disaster has several more weeks to go, even if there is no further heavy rain.<\/p>\n<!-- AddThis Advanced Settings generic via filter on the_content --><!-- AddThis Share Buttons generic via filter on the_content -->","protected":false},"excerpt":{"rendered":"<p>1. The Gansu landslide in ChinaThe rescue operations in Gansu have now clearly transitioned into a recovery and rehabilitation phase, greatly hampered by continuing very heavy rainfall in the area.&nbsp; Landslides are continuing to occur in the area, with resultant casualties. Tom Dijkstra of Loughborough University visited the site as part of a trip to look at collaborative landslide research in the area back in November.&nbsp; He has kindly sent &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":[16,59,959,10],"class_list":["post-35","post","type-post","status-publish","format-standard","hentry","category-uncategorized","tag-china","tag-flood","tag-landslide-report","tag-pakistan"],"_links":{"self":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/35","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=35"}],"version-history":[{"count":0,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/35\/revisions"}],"wp:attachment":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media?parent=35"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/categories?post=35"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/tags?post=35"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}