{"id":37950,"date":"2020-08-10T12:59:45","date_gmt":"2020-08-10T12:59:45","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=37950"},"modified":"2020-08-13T20:06:56","modified_gmt":"2020-08-13T20:06:56","slug":"mount-sinabung-eruption-in-indonesia","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/37950","title":{"rendered":"Mount Sinabung eruption in Indonesia"},"content":{"rendered":"<p><div style=\"width: 653px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/08\/200810_himawari8_trueColorRGB_Sinabung_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/08\/Himawari-8_AHI_FLDK_true_color_2020223_060000Z.png\" alt=\"Himawari-8 True Color RGB images [click to play animation | MP4]\" width=\"643\" height=\"644\" \/><\/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\/08\/200810_himawari8_trueColorRGB_Sinabung_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>displayed the gray to tan hues of a narrow west-to-east oriented volcanic ash cloud following an eruption of <a href=\"https:\/\/en.wikipedia.org\/wiki\/Mount_Sinabung\"><strong>Mount Sinabung<\/strong><\/a> on 10 August 2020.<\/p>\n<p>A sequence of Terra MODIS <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/08\/200810_0415utc_terra_modis_falseColorRGB_Sinabung.png\"><strong>False Color RGB<\/strong><\/a>, <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/08\/200810_0415utc_terra_modis_ashProbabiity_Sinabung.png\"><strong>Ash Probability<\/strong><\/a>, <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/08\/200810_0415utc_terra_modis_ashLoading_Sinabung.png\"><strong>Ash Loading<\/strong><\/a>, <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/08\/200810_0415utc_terra_modis_ashHeight_Sinabung.png\"><strong>Ash Height<\/strong><\/a> and <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/08\/200810_0415utc_terra_modis_ashEffectiveRadius_Sinabung.png\"><strong>Ash Effective Radius<\/strong><\/a> products from the <a href=\"http:\/\/volcano.ssec.wisc.edu\"><strong>NOAA\/CIMSS Volcanic Cloud Monitoring<\/strong><\/a> site<em><strong> (below)<\/strong><\/em> showed various characteristics of the ash plume at 0415 UTC.<\/p>\n<p><div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/08\/200810_0415utc_terra_modis_falseColorRGB_ashProbabilty_ashLoading_ashHeight_ashEffectiveRadius_Sinabung_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/08\/200810_0415utc_terra_modis_falseColorRGB_ashProbabilty_ashLoading_ashHeight_ashEffectiveRadius_Sinabung_anim.gif\" alt=\"Terra MODIS False Color RGB, Ash Probability, Ash Loading, Ash Height and Ash Effective Radius [click to enlarge]\" width=\"642\" height=\"527\" \/><\/a><p class=\"wp-caption-text\">Terra MODIS False Color RGB, Ash Probability, Ash Loading, Ash Height and Ash Effective Radius [click to enlarge]<\/p><\/div>A plot of 00 UTC rawinsonde data from Medan <em><strong>(below) <\/strong><\/em>helped to explain the different ash height and ash transport characteristics &#8212; the higher-altitude portion of the ash plume was transported westward by easterly flow above the 500 hPa (5.9 km) level, while the lower-altitude portion moved eastward due to westerly winds below 500 hPa.<\/p>\n<div style=\"width: 654px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/08\/200810_00UTC_WIMM_RAOB.GIF\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/08\/200810_00UTC_WIMM_RAOB.GIF\" alt=\"Plot of 00 UTC rawinsonde data from Medan, Indonesia [click to enlarge]\" width=\"644\" height=\"483\" \/><\/a><p class=\"wp-caption-text\">Plot of 00 UTC rawinsonde data from Medan, Indonesia [click to enlarge]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>JMA Himawari-8 True Color Red-Green-Blue (RGB) images created using Geo2Grid (above) displayed the gray to tan hues of a narrow west-to-east oriented volcanic ash cloud following an eruption of Mount Sinabung on 10 August 2020. A sequence of Terra MODIS False Color RGB, Ash Probability, Ash Loading, Ash Height and Ash Effective Radius products from [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":37956,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[62,12,45,71,9],"tags":[],"class_list":["post-37950","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-himawari-8","category-modis","category-redgreenblue-rgb-images","category-terra","category-volcanic-activity"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/37950","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=37950"}],"version-history":[{"count":4,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/37950\/revisions"}],"predecessor-version":[{"id":37957,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/37950\/revisions\/37957"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/37956"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=37950"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=37950"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=37950"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}