{"id":55417,"date":"2023-11-02T23:59:00","date_gmt":"2023-11-02T23:59:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=55417"},"modified":"2023-11-04T19:26:44","modified_gmt":"2023-11-04T19:26:44","slug":"eruption-of-klyuchevskaya-on-the-kamchatka-peninsula","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/55417","title":{"rendered":"Eruption of Klyuchevskaya on the Kamchatka Peninsula"},"content":{"rendered":"<p><div style=\"width: 2210px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/11\/231031_231102_himawari9_ashRGB_Klyuchevskoy_2_anim.mp4\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/11\/Himawari-9_AHI_FLDK_ash_2023305_230000Z.png\" width=\"2200\" height=\"1200\" \/><\/a><p class=\"wp-caption-text\">JMA Himawari-9 Ash RGB images, from 0000 UTC on 31 October to 2300 UTC on 02 November [click to play MP4 animation]<\/p><\/div><a href=\"https:\/\/www.jma.go.jp\/jma\/indexe.html\"><strong>JMA<\/strong><\/a> Himawari-9 <a href=\"https:\/\/rammb2.cira.colostate.edu\/wp-content\/uploads\/2020\/01\/GOES_Ash_RGB-1.pdf\"><strong>Ash RGB<\/strong><\/a> images created using <a href=\"https:\/\/www.ssec.wisc.edu\/software\/geo2grid\/\"><strong>Geo2Grid<\/strong><\/a> <em><strong>(above)<\/strong><\/em> showed<span class=\"css-901oao css-16my406 r-poiln3 r-bcqeeo r-qvutc0\"> the complex transport of <a href=\"https:\/\/en.wikipedia.org\/wiki\/Klyuchevskaya_Sopka\"><strong>Kyluchevskaya<\/strong><\/a><\/span><span class=\"css-901oao css-16my406 r-poiln3 r-bcqeeo r-qvutc0\"> volcanic plumes &#8212; which were a mixture of ash (shades of pink to red-orange) and SO2 (brighter shades of yellow) &#8212; during the 3-day period from 31 October to 02 November 2023. Much of the transport was influenced by a middle-tropospheric closed low that was progressing from Kamchatka toward the Aleutian Islands (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/11\/231031_231102_500hPa_NPacific_analyses_anim.gif\"><strong>500 hPa analyses<\/strong><\/a>).<\/span><\/p>\n<p><span class=\"css-901oao css-16my406 r-poiln3 r-bcqeeo r-qvutc0\">GOES-18 <em>(GOES-West)<\/em> <a href=\"https:\/\/rammb2.cira.colostate.edu\/wp-content\/uploads\/2020\/01\/QuickGuide_GOESR_AirMassRGB_final-1.pdf\"><strong>Air Mass RGB<\/strong><\/a> images <em><strong>(below)<\/strong><\/em> also depicted the volcanic plume &#8212; the portions that were dominated by SO2 exhibited brighter shades of pink (since the Red component of this RGB uses the <a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band10.pdf\"><strong>7.3 \u00b5m<\/strong><\/a> spectral band, which is sensitive to <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/11\/Band_10_spectral_response_SO2.jpg\"><strong>SO2 absorption<\/strong><\/a>). Volcanic Ash Advisories cautioned aviation interests of ash extending to altitudes of 36000 ft. <\/span><\/p>\n<p><div style=\"width: 1725px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/11\/231031_231102_goes18_airMassRGB_Klyuchevskoy_anim.mp4\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/11\/ak_rgb-20231101_235020.png\" alt=\"\" width=\"1715\" height=\"830\" \/><\/a><p class=\"wp-caption-text\">GOES-18 Air Mass RGB images, with plots of Pilot Reports (red) and polygons of Volcanic Ash Advisories\/Forecasts (cyan\/yellow), from 0000 UTC on 31 October to 0140 UTC on 03 November [click to play MP4 animation]<\/p><\/div>While there were very few Pilot Reports (PIREPs) in the general vicinity of the volcanic plume &#8212; since aircraft were wisely avoiding the risk of an ash encounter &#8212; there were 3 PIREPs that mentioned Volcanic Ash (VA) <em><strong>(below)<\/strong><\/em>.<\/p>\n<div style=\"width: 1926px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/11\/231031_0120utc_goes18_airMassRGB_pirep.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/11\/231031_0120utc_goes18_airMassRGB_pirep.png\" width=\"1916\" height=\"968\" \/><\/a><p class=\"wp-caption-text\">GOES-18 Air Mass RGB image at 0120 UTC on 31 October, with a Pilot Report of a thin Volcanic Ash layer at an altitude of 28000 ft [click to enlarge]<\/p><\/div>\n<div style=\"width: 1926px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/11\/231102_goes18_airMassRGB_pirep.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/11\/231102_goes18_airMassRGB_pirep.png\" width=\"1916\" height=\"968\" \/><\/a><p class=\"wp-caption-text\">GOES-18 Air Mass RGB image at 2340 UTC on 02 November, with a Pilot Report of a possible Volcanic Ash plume at an altitude of 35000 ft [click to enlarge]<\/p><\/div>\n<p><div style=\"width: 1926px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/11\/231103_goes18_airMassRGB_pirep.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/11\/231103_goes18_airMassRGB_pirep.png\" width=\"1916\" height=\"968\" \/><\/a><p class=\"wp-caption-text\">GOES-18 Air Mass RGB image at 0020 UTC on 03 November, with a Pilot Report of faint sulfur odor at Waypoint <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/11\/NATES_waypoint.png\"><strong>NATES<\/strong><\/a> (latitude\/longitude 54\u00b0N \/ 172\u00b0E), and haze below an altitude of 28000 ft [click to enlarge]<\/p><\/div>One of the more explosive events during this prolonged eruption period began around 0220 UTC on 01 November. Radiometrically-retrieved Ash Height and Ash Loading products from the <a href=\"http:\/\/volcano.ssec.wisc.edu\"><strong>NOAA\/CIMSS Volcanic Cloud Monitoring<\/strong><\/a> site are shown below &#8212; which indicated that the resulting ash-rich volcanic cloud reached heights of 10-12 km.<\/p>\n<div style=\"width: 1010px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/11\/231101_himawari9_ashHeight_Klyuchevskoy_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/11\/231101_0900utc_himawari9_ash_height.png\" width=\"1000\" height=\"821\" \/><\/a><p class=\"wp-caption-text\">Himawari-9 Ash Height derived product, from 0200-1200 UTC on 01 November [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/11\/231101_himawari9_ashHeight_Klyuchevskoy_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n<div style=\"width: 1010px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/11\/231101_himawari9_ashLoading_Klyuchevskoy_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/11\/231101_0900utc_himawari9_ash_loading.png\" width=\"1000\" height=\"821\" \/><\/a><p class=\"wp-caption-text\">Himawari-9 Ash Loading derived product, from 0200-1200 UTC on 01 November [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/11\/231101_himawari9_ashLoading_Klyuchevskoy_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>JMA Himawari-9 Ash RGB images created using Geo2Grid (above) showed the complex transport of Kyluchevskaya volcanic plumes &#8212; which were a mixture of ash (shades of pink to red-orange) and SO2 (brighter shades of yellow) &#8212; during the 3-day period from 31 October to 02 November 2023. Much of the transport was influenced by a [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":55421,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[21,114,73,45,9],"tags":[],"class_list":["post-55417","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-aviation","category-goes-18","category-himawari-9","category-redgreenblue-rgb-images","category-volcanic-activity"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/55417","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=55417"}],"version-history":[{"count":19,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/55417\/revisions"}],"predecessor-version":[{"id":55440,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/55417\/revisions\/55440"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/55421"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=55417"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=55417"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=55417"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}