{"id":35455,"date":"2020-01-19T23:59:47","date_gmt":"2020-01-19T23:59:47","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=35455"},"modified":"2020-01-22T14:55:47","modified_gmt":"2020-01-22T14:55:47","slug":"eruption-of-the-mount-shishaldin-in-alaska","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/35455","title":{"rendered":"Eruption of Mount Shishaldin in Alaska"},"content":{"rendered":"<p><div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200119_1323utc_suomiNPP_shortwaveInfrared_infraredWindow_Shishaldin_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200119_1323utc_suomiNPP_shortwaveInfrared_infraredWindow_Shishaldin_AK_anim.gif\" alt=\"Topography along with Suomi NPP VIIRS Shortwave Infrared (3.74 \u00b5m) and Infrared Window (11.45 \u00b5m) images at 1323 UTC [click to enlarge]\" width=\"642\" height=\"368\" \/><\/a><p class=\"wp-caption-text\">Topography along with Suomi NPP VIIRS Shortwave Infrared <em>(3.74 \u00b5m)<\/em> and Infrared Window <em>(11.45 \u00b5m)<\/em> images at 1323 UTC [click to enlarge]<\/p><\/div>Following two days of increasing seismicity, <a href=\"https:\/\/en.wikipedia.org\/wiki\/Mount_Shishaldin\"><strong>Mount Shishaldin<\/strong><\/a> began a period of more intense eruptive activity around 0930 UTC on 19 January 2020 &#8212; a comparison of topography along with Suomi NPP VIIRS Shortwave Infrared (3.74 \u00b5m) and Infrared Window (11.45 \u00b5m) images at 1323 UTC<em><strong> (above)<\/strong><\/em> displayed a distinct thermal anomaly <em>(cluster of red 3.74 \u00b5m pixels)<\/em> and a volcanic cloud moving east-southeastward.<\/p>\n<p>Comparisons of Shortwave Infrared and Infrared Window images from Suomi NPP VIIRS and GOES-17 ABI<strong> <em>(below)<\/em><\/strong> revealed a <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/217\"><strong>parallax<\/strong><\/a> shift that is inherent with geostationary imagery at high latitudes.<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200119_1323utc_suomiNPP_goes17_shortwaveInfrared_Shishaldin_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200119_1323utc_suomiNPP_goes17_shortwaveInfrared_Shishaldin_AK_anim.gif\" alt=\"Comparison of Shortwave Infrared images from Suomi NPP VIIRS (3.74 um) and GOES-17 ABI (3.9 um) [click to enlarge]\" width=\"640\" height=\"366\" \/><\/a><p class=\"wp-caption-text\">Comparison of Shortwave Infrared images from Suomi NPP VIIRS <em>(3.74 \u00b5m)<\/em> and GOES-17 ABI <em>(3.9 \u00b5m)<\/em> [click to enlarge]<\/p><\/div><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200119_1323utc_suomiNPP_goes17_infraredWindow_Shishaldin_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200119_1323utc_suomiNPP_goes17_infraredWindow_Shishaldin_AK_anim.gif\" alt=\"Comparison of Infrared Window images from Suomi NPP VIIRS (11.45 \u00b5m) and GOES-17 ABI (10.35 \u00b5m) [click to enlarge]\" width=\"641\" height=\"367\" \/><\/a><p class=\"wp-caption-text\">Comparison of Infrared Window images from Suomi NPP VIIRS <em>(11.45 \u00b5m)<\/em> and GOES-17 ABI <em>(10.35 \u00b5m)<\/em> [click to enlarge]<\/p><\/div>A toggle between GOES-17 <a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/webapps\/parallax\/overview.html\"><strong>parallax correction<\/strong><\/a> vectors and magnitudes for cloud top heights of 15,000 feet (4.5 km) and 30,000 feet (9.1 km) are shown below &#8212;\u00a0 the amount of northwestward volcanic cloud displacement between the Suomi NPP and GOES-17 Infrared images roughly matched the 16 km (or 10 mile) value for a 15,000 foot cloud top in that region of the Full Disk. <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200119_Shishaldin_advisories.text\"><strong>Later advisories<\/strong><\/a> listed the maximum ash height at 20,000-30,0000 feet.<\/p>\n<p><div style=\"width: 653px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/GOES-17_parallax_15kft_30kft_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/GOES-17_parallax_15kft_30kft_anim.gif\" alt=\"GOES-17 parallax correction vectors (green) and magnitudes (km, red) [click to enlarge]\" width=\"643\" height=\"336\" \/><\/a><p class=\"wp-caption-text\">GOES-17 parallax correction vectors <em>(green)<\/em> and magnitudes<em> (km, red)<\/em> [click to enlarge]<\/p><\/div>1-minute <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/23225\"><strong>Mesoscale Domain Sector<\/strong><\/a> GOES-17 <em>(GOES-West)<\/em> <a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_G16_CloudPhaseBTD.pdf\"><strong>Split Cloud Top Phase<\/strong><\/a> (11.2 &#8211; 8.4 \u00b5m) images <em><strong>(below)<\/strong><\/em> displayed an increasing volcanic ash signal<em> (negative values, darker blue to violet enhancement)<\/em> beginning around 01 UTC on 20 January. Some light ash fall was reported at False Pass, Alaska.<\/p>\n<p><div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200119_goes17_splitCloudTopPhase_Shishaldin_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/ak_ctp-20200120_040059.png\" alt=\"GOES-17 Split Cloud Top Phase (11.2 - 8.4 um) images [click to play animation | MP4]\" width=\"642\" height=\"368\" \/><\/a><p class=\"wp-caption-text\">GOES-17 Split Cloud Top Phase <em>(11.2 &#8211; 8.4 \u00b5m)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200119_goes17_splitCloudTopPhase_Shishaldin_AK_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>10-minute images of GOES-17 radiometrially retreived Ash Height from the <a href=\"https:\/\/volcano.ssec.wisc.edu\/\"><strong>NOAA\/CIMSS Volcanic Cloud<\/strong><\/a> monitoring site <em><strong>(below)<\/strong><\/em> indicated that the bulk of the ash plume existed within the 2-6 km altitude range.<\/p>\n<p><div style=\"width: 653px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200119_goes17_ash_height_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/haimage_12.png\" alt=\"GOES-17 Ash Height product [click to play animation | MP4]\" width=\"643\" height=\"527\" \/><\/a><p class=\"wp-caption-text\">GOES-17 Ash Height product [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200119_goes17_ash_height_AK_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>In corresponding GOES-17 False Color Red-Green-Blue (RGB) images <em><strong>(below)<\/strong>,<\/em> the volcanic plume exhibited shades of red\/magenta\/pink &#8212; the characteristic signature of an ash-laden cloud.<\/p>\n<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200119_goes17_rgb_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/haimage_rgb_12.png\" alt=\"GOES-17 False Color RGB [click to play animation | MP4]\" width=\"640\" height=\"525\" \/><\/a><p class=\"wp-caption-text\">GOES-17 False Color RGB [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200119_goes17_rgb_AK_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>Following two days of increasing seismicity, Mount Shishaldin began a period of more intense eruptive activity around 0930 UTC on 19 January 2020 &#8212; a comparison of topography along with Suomi NPP VIIRS Shortwave Infrared (3.74 \u00b5m) and Infrared Window (11.45 \u00b5m) images at 1323 UTC (above) displayed a distinct thermal anomaly (cluster of red [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":35463,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[80,45,49,48,9],"tags":[],"class_list":["post-35455","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-17","category-redgreenblue-rgb-images","category-suomi_npp","category-viirs","category-volcanic-activity"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/35455","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=35455"}],"version-history":[{"count":13,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/35455\/revisions"}],"predecessor-version":[{"id":35471,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/35455\/revisions\/35471"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/35463"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=35455"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=35455"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=35455"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}