{"id":43894,"date":"2021-12-19T23:59:00","date_gmt":"2021-12-19T23:59:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=43894"},"modified":"2022-12-10T00:14:36","modified_gmt":"2022-12-10T00:14:36","slug":"eruption-of-the-hunga-tonga-hunga-haapai-volcano","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/43894","title":{"rendered":"Eruption of the Hunga Tonga-Hunga Ha&#8217;apai volcano"},"content":{"rendered":"<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211219_himawari8_ashHeight_Tonga_volcano_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211219_2200z_height.png\" width=\"640\" height=\"580\" \/><\/a><p class=\"wp-caption-text\">Ash Height product [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211219_himawari8_ashHeight_Tonga_volcano_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n<p>The <b><a href=\"https:\/\/en.wikipedia.org\/wiki\/Hunga_Tonga\">Hunga Tonga-Hunga Ha?apai<\/a><\/b> volcano in Tonga violently erupted around 2030 UTC on 19 December 2021 &#8212; and a radiometrically-retrieved Ash Height product from the <a href=\"http:\/\/volcano.ssec.wisc.edu\"><strong>NOAA\/CIMSS Volcanic Cloud Monitoring<\/strong><\/a> site (using <a href=\"https:\/\/www.jma.go.jp\/jma\/indexe.html\"><strong>JMA<\/strong><\/a> Himawari-8 data) indicated that ash was ejected as high as 16-18 km <em><strong>(above)<\/strong><\/em>.<\/p>\n<p>Ash Loading was very high within the volcanic cloud, with particles having a large Ash Effective Radius <em><strong>(below)<\/strong><\/em>.<\/p>\n<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211219_himawari8_ashLoading_Tonga_volcano_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211219_2200z_loading.png\" width=\"640\" height=\"580\" \/><\/a><p class=\"wp-caption-text\">Ash Loading product [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211219_himawari8_ashLoading_Tonga_volcano_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n<p>\u00a0<\/p>\n<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211219_himawari8_ashEffectiveRadius_Tonga_volcano_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211219_2200z_radius.png\" width=\"640\" height=\"580\" \/><\/a><p class=\"wp-caption-text\">Ash Effective Radius product [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211219_himawari8_ashEffectiveRadius_Tonga_volcano_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n<p>In GOES-17 <em>(GOES-East)<\/em> <a href=\"https:\/\/rammb.cira.colostate.edu\/training\/visit\/quick_guides\/GOES_Ash_RGB.pdf\"><strong>Ash RGB<\/strong><\/a> images created using <a href=\"https:\/\/www.ssec.wisc.edu\/software\/geo2grid\/\"><strong>Geo2Grid<\/strong><\/a> <em><strong>(below)<\/strong><\/em>, brighter shades of yellow indicated that significant concentrations of SO2 were present within the volcanic cloud &#8212; while shades of red supported the presence of ash.<\/p>\n<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211219_goes17_ashRGB_Tonga_volcano_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/GOES-17_ABI_RadF_ash_2021353_213031Z.png\" width=\"640\" height=\"640\" \/><\/a><p class=\"wp-caption-text\">GOES-17 Ash RGB images [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211219_goes17_ashRGB_Tonga_volcano_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n<p>GOES-17 <a href=\"https:\/\/rammb.cira.colostate.edu\/training\/visit\/quick_guides\/QuickGuide_DayCloudPhaseDistinction_final_v2.pdf\"><strong>Day Cloud Phase Distinction RGB<\/strong><\/a> images <em><strong>(below)<\/strong><\/em> clearly showed the expansion of the glaciated volcanic cloud (brighter shades of orange).<\/p>\n<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211219_goes17_dayMicrophysicsRGB_Tonga_volcano_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/GOES-17_ABI_RadF_day_microphysics_2021353_220032Z.png\" width=\"640\" height=\"640\" \/><\/a><p class=\"wp-caption-text\">GOES-17 Day Cloud Phase Distinction RGB images (credit: Tim Schmit, NOAA\/NESDIS\/ASPB) [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211219_goes17_dayMicrophysicsRGB_Tonga_volcano_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n<p>GOES-17 &#8220;Clean&#8221; Infrared Window (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band13.pdf\"><strong>10.35 \u00b5m<\/strong><\/a>) images <em><strong>(below)<\/strong><\/em> indicated that the coldest cloud-top infrared brightness temperatures were in the -80 to -89C range (shades of violet).<\/p>\n<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211219_goes17_infrared_Tonga_volcano_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/G17_IR_TONGA_VOLCANO_19DEC2021_B13_2021353_221032_GOES-17_0001PANEL_FRAME0000012.GIF\" width=\"640\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">GOES-17 &#8220;Clean&#8221; Infrared Window (10.35 \u00b5m) images [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211219_goes17_infrared_Tonga_volcano_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n\n\n<figure class=\"wp-block-embed is-type-rich is-provider-twitter wp-block-embed-twitter\"><div class=\"wp-block-embed__wrapper\">\n<blockquote class=\"twitter-tweet\" data-width=\"500\" data-dnt=\"true\"><p lang=\"en\" dir=\"ltr\">Here&#39;s another cool view of the Tonga volcanic eruption <br><br>This is how two different satellites saw it, at exactly the same time. Nice pseudo-3d effect! <a href=\"https:\/\/t.co\/iswrCaJMpX\">https:\/\/t.co\/iswrCaJMpX<\/a> <a href=\"https:\/\/t.co\/M8xInwyXl6\">pic.twitter.com\/M8xInwyXl6<\/a><\/p>&mdash; Simon Proud (@simon_sat) <a href=\"https:\/\/twitter.com\/simon_sat\/status\/1472896286001090564?ref_src=twsrc%5Etfw\">December 20, 2021<\/a><\/blockquote><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script>\n<\/div><\/figure>\n","protected":false},"excerpt":{"rendered":"<p>The Hunga Tonga-Hunga Ha?apai volcano in Tonga violently erupted around 2030 UTC on 19 December 2021 &#8212; and a radiometrically-retrieved Ash Height product from the NOAA\/CIMSS Volcanic Cloud Monitoring site (using JMA Himawari-8 data) indicated that ash was ejected as high as 16-18 km (above). Ash Loading was very high within the volcanic cloud, with [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":43911,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[132,80,62,45,9],"tags":[],"class_list":["post-43894","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-geo2grid","category-goes-17","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\/43894","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=43894"}],"version-history":[{"count":11,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/43894\/revisions"}],"predecessor-version":[{"id":49151,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/43894\/revisions\/49151"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/43911"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=43894"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=43894"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=43894"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}