{"id":39087,"date":"2020-11-29T16:07:50","date_gmt":"2020-11-29T16:07:50","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=39087"},"modified":"2020-12-04T17:05:59","modified_gmt":"2020-12-04T17:05:59","slug":"eruption-of-the-lewotolok-volcano-in-indonesia","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/39087","title":{"rendered":"Eruption of the Lewotolok volcano in Indonesia"},"content":{"rendered":"<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/11\/201129_himawari_trueColorRGB_Lewotolok_eruption_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/11\/Himawari-8_AHI_FLDK_true_color_2020334_032000Z.png\" alt=\"Himawari-8 True Color RGB images [click to play animation | MP4]\" width=\"640\" height=\"640\" \/><\/a><p class=\"wp-caption-text\">Himawari-8 True Color RGB images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/11\/201129_himawari_trueColorRGB_Lewotolok_eruption_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div><a href=\"https:\/\/www.jma.go.jp\/jma\/indexe.html\"><strong>JMA<\/strong><\/a> Himawari-8 True Color Red-Green-Blue (RGB) images created using <a href=\"https:\/\/www.ssec.wisc.edu\/software\/geo2grid\/\"><strong>Geo2Grid<\/strong><\/a> <em><strong>(above)<\/strong><\/em> showed the volcanic clouds produced by an eruption of <a href=\"https:\/\/en.wikipedia.org\/wiki\/Mount_Ile_Lewotolok\"><strong>Lewotolok<\/strong><\/a> in Indonesia on 29 November 2020 &#8212; with one cloud plume moving to the northwest, and another moving more rapidly southeastward. This difference in volcanic cloud propagation was due to directional wind shear, as revealed by <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/11\/201129_00UTC_WRKK_RAOB_DATA.TEXT\"><strong>rawinsonde data<\/strong><\/a> from Kupang on the island of Timor <em><strong>(below)<\/strong>,<\/em> located about 250 km southeast of Lewotolok. A shift to northwesterly winds occurred at an altitude around 9 km (the 322 hPa pressure level).<\/p>\n<div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/11\/201129_00UTC_WRKK_RAOB.GIF\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/11\/201129_00UTC_WRKK_RAOB.GIF\" alt=\"Plot of rawinsonde data from Kupang, Indonesia [click to enlarge]\" width=\"641\" height=\"481\" \/><\/a><p class=\"wp-caption-text\">Plot of rawinsonde data from Kupang, Indonesia [click to enlarge]<\/p><\/div>\n<p><div style=\"width: 654px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/11\/201129_himawari_ashRGB_Lewotolok_eruption_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/11\/Himawari-8_AHI_FLDK_ash_2020334_032000Z.png\" alt=\"Himawari-8 Ash RGB images [click to play animation | MP4]\" width=\"644\" height=\"644\" \/><\/a><p class=\"wp-caption-text\">Himawari-8 Ash RGB images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/11\/201129_himawari_ashRGB_Lewotolok_eruption_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>Himawari-8 Ash RGB images <em><strong>(above)<\/strong><\/em> displayed an ash signature for both volcanic plumes, which became more diffuse after about 5 hours. Himawari-8 retrievals of Ash Height from the <a href=\"http:\/\/volcano.ssec.wisc.edu\"><strong>NOAA\/CIMSS Volcanic Cloud Monitoring<\/strong><\/a> site <em><strong>(below)<\/strong><\/em> showed maximum values in the 16-18 km range for the southeast-moving cloud (the\u00a0 <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/11\/201129_0420utc_Lewotolo_advisory.png\"><strong>advisory<\/strong><\/a> issued by the <a href=\"http:\/\/www.bom.gov.au\/aviation\/volcanic-ash\/\"><strong>Darwin VAAC<\/strong><\/a> listed maximum height values of 50,000 feet or 15 km).<\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/11\/201129_himawari8_ashHeight_Lewotolok_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/11\/201129_0400utc_himawari8_ash_height.png\" alt=\"Himawari-8 Ash Height [click to play animation | MP4]\" width=\"641\" height=\"526\" \/><\/a><p class=\"wp-caption-text\">Himawari-8 Ash Height [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/11\/201129_himawari8_ashHeight_Lewotolok_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>Himawari-8 False Color images <em><strong>(below)<\/strong><\/em> indicated the presence of both SO2<em> (shades of yellow to green)<\/em> <strong>and<\/strong> ash in the southeastward-moving volcanic cloud.<\/p>\n<p><div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/11\/201129_himawari8_so2RGB_Lewotolok_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/11\/201129_0400utc_himawari8_so2RGB.png\" alt=\"Himawari-8 False Color images [click to play animation | MP4]\" width=\"642\" height=\"527\" \/><\/a><p class=\"wp-caption-text\">Himawari-8 False Color images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/11\/201129_himawari8_so2RGB_Lewotolok_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div><center><\/p>\n<blockquote class=\"twitter-tweet\">\n<p dir=\"ltr\" lang=\"en\">Explosive <a href=\"https:\/\/twitter.com\/hashtag\/eruption?src=hash&amp;ref_src=twsrc%5Etfw\">#eruption<\/a> of <a href=\"https:\/\/twitter.com\/hashtag\/Lewotolo?src=hash&amp;ref_src=twsrc%5Etfw\">#Lewotolo<\/a> (<a href=\"https:\/\/twitter.com\/hashtag\/Lewotolok?src=hash&amp;ref_src=twsrc%5Etfw\">#Lewotolok<\/a>) <a href=\"https:\/\/twitter.com\/hashtag\/volcano?src=hash&amp;ref_src=twsrc%5Etfw\">#volcano<\/a>, E. <a href=\"https:\/\/twitter.com\/hashtag\/Indonesia?src=hash&amp;ref_src=twsrc%5Etfw\">#Indonesia<\/a>, at 01:50 UTC on Nov 29. Rapidly identified by the <a href=\"https:\/\/twitter.com\/NOAA?ref_src=twsrc%5Etfw\">@NOAA<\/a>\/<a href=\"https:\/\/twitter.com\/UWCIMSS?ref_src=twsrc%5Etfw\">@UWCIMSS<\/a> VOLCAT system due to strong thermal signal and vertical Cloud Growth Anomaly (<a href=\"https:\/\/twitter.com\/hashtag\/VolcanoCb?src=hash&amp;ref_src=twsrc%5Etfw\">#VolcanoCb<\/a>) in <a href=\"https:\/\/twitter.com\/hashtag\/Himawari?src=hash&amp;ref_src=twsrc%5Etfw\">#Himawari<\/a> imagery. Max ash cloud height &gt;12 km. <a href=\"https:\/\/t.co\/qoPcTlFJpz\">pic.twitter.com\/qoPcTlFJpz<\/a><\/p>\n<p>\u2014 Simon Carn (@simoncarn) <a href=\"https:\/\/twitter.com\/simoncarn\/status\/1332894551258882048?ref_src=twsrc%5Etfw\">November 29, 2020<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><br \/>\n<\/center><\/p>\n","protected":false},"excerpt":{"rendered":"<p>JMA Himawari-8 True Color Red-Green-Blue (RGB) images created using Geo2Grid (above) showed the volcanic clouds produced by an eruption of Lewotolok in Indonesia on 29 November 2020 &#8212; with one cloud plume moving to the northwest, and another moving more rapidly southeastward. This difference in volcanic cloud propagation was due to directional wind shear, as [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":39111,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[62,45,9],"tags":[],"class_list":["post-39087","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-himawari-8","category-redgreenblue-rgb-images","category-volcanic-activity"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/39087","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/users\/18"}],"replies":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/comments?post=39087"}],"version-history":[{"count":7,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/39087\/revisions"}],"predecessor-version":[{"id":39136,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/39087\/revisions\/39136"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/39111"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=39087"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=39087"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=39087"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}