{"id":36700,"date":"2021-02-15T08:16:54","date_gmt":"2021-02-15T08:16:54","guid":{"rendered":"https:\/\/blogs.agu.org\/landslideblog\/?p=36700"},"modified":"2021-02-15T08:16:54","modified_gmt":"2021-02-15T08:16:54","slug":"perspectives-on-the-chamoli-debris-flow-disaster-in-uttarakhand","status":"publish","type":"post","link":"https:\/\/blogs.agu.org\/landslideblog\/2021\/02\/15\/perspectives-on-the-chamoli-debris-flow-disaster-in-uttarakhand\/","title":{"rendered":"New perspectives on the Chamoli debris flow disaster"},"content":{"rendered":"<h4>New perspectives on the Chamoli debris flow disaster<\/h4>\n<p>The grim search for the victims of the <a href=\"https:\/\/blogs.agu.org\/landslideblog\/2021\/02\/08\/chamoli-2\/\">Chamoli debris flow disaster in Uttarakhand in India<\/a> is continuing, with much of the effort being focused on the tunnels associated with the Tapovan Vishnugad hydroelectric scheme.\u00a0 As of this morning (15 February 2021), <a href=\"https:\/\/in.news.yahoo.com\/chamoli-glacier-burst-death-toll-065705215.html?guccounter=1&amp;guce_referrer=aHR0cHM6Ly93d3cuZ29vZ2xlLmNvbS8&amp;guce_referrer_sig=AQAAAEdXUc3_jnTeCnL1DODHoWTdhCfd2HuPxGmTcMRQsf5DUT1nw6fsI8eRefmkR1RMB8qNviFHbCKAOej9WxnjnD8MdwkO5xbkX5Gqz6iOmcEx-uu-jx0TX0e07Ej0BoAYHigz1pcX7EPHq_700Lp2FGlA98PHAVm1TqUbTCo_-4cE\">54 people are known to have lost their lives and 179 people are reported to be missing<\/a>.\u00a0 The Tapovan tunnel operation is extremely challenging as it is filled with sediment, including large boulders.<\/p>\n<p>The <a href=\"https:\/\/blogs.agu.org\/landslideblog\/2021\/02\/11\/chamoli-landslide-3\/\">Planet Labs high resolution images are incredible<\/a> &#8211; it is almost impossible to do them justice.\u00a0 I have imported them into Google Earth and draped them onto the landscape, which helps to provide a perspective on the events.\u00a0 The image below shows the slope that failed, taken a few days before the landslide:<\/p>\n<p>&nbsp;<\/p>\n<div id=\"attachment_36703\" style=\"width: 809px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-36703\" class=\" wp-image-36703\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/21_02-Chamoli-8-scaled.jpg\" alt=\"The site of the Chamoli landslide\" width=\"799\" height=\"548\" srcset=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/21_02-Chamoli-8-scaled.jpg 2560w, https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/21_02-Chamoli-8-300x206.jpg 300w, https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/21_02-Chamoli-8-1024x702.jpg 1024w, https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/21_02-Chamoli-8-768x527.jpg 768w, https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/21_02-Chamoli-8-1536x1053.jpg 1536w, https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/21_02-Chamoli-8-2048x1404.jpg 2048w\" sizes=\"auto, (max-width: 799px) 100vw, 799px\" \/><p id=\"caption-attachment-36703\" class=\"wp-caption-text\">Google Earth perspective view of the slope that failed in the Chamoli landslide<\/p><\/div>\n<p>.<\/p>\n<p>The terrain was steep and barren, with some woodland in the lower parts of the valley.\u00a0 The image below shows the same view, but with the <a href=\"https:\/\/www.planet.com\/\">Planet Labs<\/a> SkySat image draped onto the topography:-<\/p>\n<div id=\"attachment_36705\" style=\"width: 803px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-36705\" class=\" wp-image-36705\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/21_02-Chamoli-9-scaled.jpg\" alt=\"Planets Labs imagery of the Chamoli landslide\" width=\"793\" height=\"538\" srcset=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/21_02-Chamoli-9-scaled.jpg 2560w, https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/21_02-Chamoli-9-300x204.jpg 300w, https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/21_02-Chamoli-9-1024x695.jpg 1024w, https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/21_02-Chamoli-9-768x522.jpg 768w, https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/21_02-Chamoli-9-1536x1043.jpg 1536w, https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/21_02-Chamoli-9-2048x1391.jpg 2048w\" sizes=\"auto, (max-width: 793px) 100vw, 793px\" \/><p id=\"caption-attachment-36705\" class=\"wp-caption-text\">Google Earth perspective view of the slope that failed in the Chamoli landslide, with the <a href=\"https:\/\/www.planet.com\/\">Planet Labs<\/a> SkySat imagery draped over. Imagery copyright <a href=\"https:\/\/www.planet.com\/\">Planet Labs<\/a>, used with permission.<\/p><\/div>\n<p>.<\/p>\n<p>To provide a comparison, I have created a slider below that allows you to flick between the images:-<\/p>\n<div class=\"juxtapose\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/21_02-Chamoli-8-scaled.jpg\" alt=\"The site of the Chamoli landslide\" width=\"799\" height=\"548\" \/><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/21_02-Chamoli-9-scaled.jpg\" alt=\"Planets Labs imagery of the Chamoli landslide\" width=\"793\" height=\"538\" \/><\/div>\n<p>.<\/p>\n<p>The large block that has failed is clearly seen in the later image, as is the very steep slope down which the debris travelled. The debris appears to have travelled some distance up the opposite slope before heading down the valley.\u00a0 The image below uses the lower resolution <a href=\"https:\/\/www.planet.com\/\">Planet Labs<\/a> PlanetScope imagery to show the path of the debris:<\/p>\n<div id=\"attachment_36707\" style=\"width: 809px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-36707\" class=\" wp-image-36707\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/21_02-Chamoli-10-scaled.jpg\" alt=\"The path of the debris that formed the Chamoli debris flow\" width=\"799\" height=\"543\" srcset=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/21_02-Chamoli-10-scaled.jpg 2560w, https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/21_02-Chamoli-10-300x204.jpg 300w, https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/21_02-Chamoli-10-1024x696.jpg 1024w, https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/21_02-Chamoli-10-768x522.jpg 768w, https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/21_02-Chamoli-10-1536x1044.jpg 1536w, https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/21_02-Chamoli-10-2048x1391.jpg 2048w\" sizes=\"auto, (max-width: 799px) 100vw, 799px\" \/><p id=\"caption-attachment-36707\" class=\"wp-caption-text\">The path of the debris that formed the Chamoli debris flow. Imagery copyright <a href=\"https:\/\/www.planet.com\/\">Planet Labs<\/a>, used with permission.<\/p><\/div>\n<p>.<\/p>\n<p>The area of dust deposition in the upper part of the flow path is clear.\u00a0 It appears that the flow became increasingly confined to the lower part of te valley, possibly as it transitioned into a debris flow.<\/p>\n<p>The image below, which was prepared by my friends at <a href=\"https:\/\/www.planet.com\/\">Planet Labs<\/a>, show the full path of the Chamoli landslide and debris flow to the Tapovan Vishnugad hydroelectric dam site:<\/p>\n<div id=\"attachment_36709\" style=\"width: 810px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-36709\" class=\" wp-image-36709\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/rockfall_flood_chamoli_india__0002_20210208_2276_3B_AnalyticMS_rgb_alt_crop_5292_flat_wm_ANNOTATED-scaled.jpg\" alt=\"The track of the Chamoli landslide and debris flow\" width=\"800\" height=\"1005\" srcset=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/rockfall_flood_chamoli_india__0002_20210208_2276_3B_AnalyticMS_rgb_alt_crop_5292_flat_wm_ANNOTATED-scaled.jpg 2037w, https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/rockfall_flood_chamoli_india__0002_20210208_2276_3B_AnalyticMS_rgb_alt_crop_5292_flat_wm_ANNOTATED-239x300.jpg 239w, https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/rockfall_flood_chamoli_india__0002_20210208_2276_3B_AnalyticMS_rgb_alt_crop_5292_flat_wm_ANNOTATED-815x1024.jpg 815w, https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/rockfall_flood_chamoli_india__0002_20210208_2276_3B_AnalyticMS_rgb_alt_crop_5292_flat_wm_ANNOTATED-768x965.jpg 768w, https:\/\/blogs.agu.org\/landslideblog\/files\/2021\/02\/rockfall_flood_chamoli_india__0002_20210208_2276_3B_AnalyticMS_rgb_alt_crop_5292_flat_wm_ANNOTATED-1222x1536.jpg 1222w\" sizes=\"auto, (max-width: 800px) 100vw, 800px\" \/><p id=\"caption-attachment-36709\" class=\"wp-caption-text\">The track of the Chamoli landslide and debris flow. Image prepared by <a href=\"https:\/\/www.planet.com\/\">Planet Labs<\/a>, used with permission.<\/p><\/div>\n<p>.<\/p>\n<h4>Reference<\/h4>\n<p>Planet Team (2021). Planet Application Program Interface: In Space for Life on Earth. San Francisco, CA. <a href=\"https:\/\/www.planet.com\/\">https:\/\/www.planet.com\/<\/a><\/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>New perspectives on the Chamoli debris flow disaster in Uttarakhand provided by the high resolution Planet Labs imagery <!-- 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":36707,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[7203],"tags":[30614,469,913,5,1205,25,72],"class_list":["post-36700","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-planet-labs","tag-chamoli","tag-featured","tag-hydroelectric","tag-india","tag-planet-labs","tag-satellite","tag-south-asia"],"_links":{"self":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/36700","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=36700"}],"version-history":[{"count":0,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/36700\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media\/36707"}],"wp:attachment":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media?parent=36700"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/categories?post=36700"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/tags?post=36700"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}