{"id":55109,"date":"2023-10-10T23:59:00","date_gmt":"2023-10-10T23:59:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=55109"},"modified":"2023-10-13T22:02:18","modified_gmt":"2023-10-13T22:02:18","slug":"resuspended-volcanic-ash-from-the-1912-novarupta-katmai-eruption","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/55109","title":{"rendered":"Resuspended volcanic ash from the 1912 Novarupta-Katmai eruption"},"content":{"rendered":"<p><div style=\"width: 1725px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/10\/231010_goes18_dustRGB_Katmai_resuspended_ash_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/10\/ak_rgb-20231010_132021.png\" width=\"1715\" height=\"830\" \/><\/a><p class=\"wp-caption-text\">GOES-18 Dust RGB images, from 2330 UTC on 09 October to 0100 UTC on 11 October [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/10\/231005_231011_Atlantic_surface_analyses_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>GOES-18 <em>(GOES-West)<\/em>\u00a0<a href=\"https:\/\/rammb.cira.colostate.edu\/training\/visit\/quick_guides\/Dust_RGB_Quick_Guide.pdf\"><strong>Dust RGB<\/strong><\/a>\u00a0images\u00a0<em><strong>(above)<\/strong><\/em> showed a plume of resuspended volcanic ash (brighter shades of pink) from the <a href=\"https:\/\/en.wikipedia.org\/wiki\/Novarupta\"><strong>1912 Novarupta-Katmai<\/strong><\/a>\u00a0eruption in Alaska, which was being transported offshore across the\u00a0<a href=\"https:\/\/en.wikipedia.org\/wiki\/Shelikof_Strait\"><strong>Shelikof Strait<\/strong><\/a> (and <a href=\"https:\/\/www.ndbc.noaa.gov\/station_page.php?station=46077\"><strong>Buoy 46077<\/strong><\/a>, where the <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/10\/231011_buoy46077_peak_wind_gust.png\"><strong>peak wind gusts<\/strong><\/a> were 31 knots) toward Kodiak Island on 10 October 2023. Surface ash within the <a href=\"https:\/\/en.wikipedia.org\/wiki\/Valley_of_Ten_Thousand_Smokes\"><strong>Valley Of Ten Thousand Smokes<\/strong><\/a> was being lofted by a burst of strong northwesterly winds &#8212; a toggle between the 1200 UTC Dust RGB image and Topography <em><strong>(below)<\/strong><\/em> highlighted the valleys associated with the ash source region.<\/p>\n<p><div style=\"width: 1725px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/10\/231010_1200utc_goes18_dustRGB_topography_Katmai_resuspended_ash_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/10\/231010_1200utc_goes18_dustRGB_topography_Katmai_resuspended_ash_anim.gif\" width=\"1715\" height=\"830\" \/><\/a><p class=\"wp-caption-text\">GOES-18 Dust RGB and Topography images [click to enlarge]<\/p><\/div>As the plume of resuspended ash moved over the northern portion of Kodiak Island, the Kodiak Airport (PADQ) began to report Volcanic Ash (VA) at 1900 UTC <em><strong>(below)<\/strong><\/em> &#8212; and the ash plume briefly restricted the surface visibility to 8 miles at <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/10\/ak_rgb-20231010_201021.png\"><strong>2200 UTC<\/strong><\/a>.<\/p>\n<p><div style=\"width: 1550px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/10\/231010_1900utc_goes18_dustRGB_padq_metar.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/10\/231010_1900utc_goes18_dustRGB_padq_metar.png\" width=\"1540\" height=\"781\" \/><\/a><p class=\"wp-caption-text\">GOES-18 Dust RGB image at 1900 UTC, with a cursor sample of the Kodiak Airport METAR report [click to enlarge]<\/p><\/div>While a signature of the plume was also evident in GOES-18 <a href=\"https:\/\/rammb2.cira.colostate.edu\/wp-content\/uploads\/2020\/01\/GOES_Ash_RGB-1.pdf\"><strong>Ash RGB<\/strong><\/a> imagery, it was more obvious in the Dust RGB <em><strong>(below) <\/strong><\/em>&#8212; both RGBs use the same spectral bands and spectral band differences, but the individual RGB components are scaled differently (so an examination of both is advised, in order to determine which RGB is best to track an ash-related feature).<\/p>\n<p><div style=\"width: 1725px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/10\/231010_1200utc_dustRGB_ashRGB_Katmai_resuspended_ash_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/10\/231010_1200utc_dustRGB_ashRGB_Katmai_resuspended_ash_anim.gif\" width=\"1715\" height=\"830\" \/><\/a><p class=\"wp-caption-text\">GOES-18 Dust RGB and Ash RGB images at 1200 UTC [click to enlarge]<\/p><\/div>GOES-18 daytime True Color RGB + <a href=\"https:\/\/rammb.cira.colostate.edu\/training\/visit\/quick_guides\/QuickGuide_GOESR_NtMicroRGB_Final_20191206.pdf\"><strong>Nighttime Microphysics RGB<\/strong><\/a> images from the <a href=\"https:\/\/geosphere.ssec.wisc.edu\/#playing:true;coordinate:0,46783;zoom:0.8;satellite:goeswest;num_frames:30;\"><strong>CSPP GeoSphere<\/strong><\/a>\u00a0site\u00a0<em><strong>(below)<\/strong><\/em> provided another view of the resuspended ash plume.<\/p>\n<div style=\"width: 1034px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/10\/231009_2300utc_231011_0100utc_goes18_nighttimeMicrophysicsRGB_trueColorRGB_Katmai_resuspended_ash_anim.mp4\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/10\/goeswest_abi_radf_true_color_night_20231010190021.png\" alt=\"\" width=\"1024\" height=\"461\" \/><\/a><p class=\"wp-caption-text\">GOES-18 daytime True Color RGB and Nighttime Microphysics RGB images [click to play MP4 animation]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>GOES-18 (GOES-West)\u00a0Dust RGB\u00a0images\u00a0(above) showed a plume of resuspended volcanic ash (brighter shades of pink) from the 1912 Novarupta-Katmai\u00a0eruption in Alaska, which was being transported offshore across the\u00a0Shelikof Strait (and Buoy 46077, where the peak wind gusts were 31 knots) toward Kodiak Island on 10 October 2023. Surface ash within the Valley Of Ten Thousand Smokes [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":55112,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[114,45],"tags":[],"class_list":["post-55109","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-18","category-redgreenblue-rgb-images"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/55109","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=55109"}],"version-history":[{"count":16,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/55109\/revisions"}],"predecessor-version":[{"id":55142,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/55109\/revisions\/55142"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/55112"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=55109"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=55109"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=55109"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}