{"id":17179,"date":"2014-11-15T23:59:56","date_gmt":"2014-11-15T23:59:56","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=17179"},"modified":"2014-11-17T16:26:54","modified_gmt":"2014-11-17T16:26:54","slug":"eruption-of-the-pavlof-volcano-in-alaska","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/17179","title":{"rendered":"Eruption of the Pavlof Volcano in Alaska"},"content":{"rendered":"<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/11\/141114_1307z_suomi_npp_viirs_dnb_swir_Pavlof_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/11\/141114_1307z_suomi_npp_viirs_dnb_swir_Pavlof_anim.gif\" alt=\"Suomi NPP VIIRS 0.7 \u00b5m Day\/Night Band and 3.74 \u00b5m shortwave IR images\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS 0.7 \u00b5m Day\/Night Band and 3.74 \u00b5m shortwave IR images<\/p><\/div>\n<p>According to the <a title=\"Alaska Volcano Observatory\" href=\"http:\/\/www.avo.alaska.edu\/\"><strong>Alaska Volcano Observatory<\/strong><\/a>, an eruption of the <a title=\"Pavlof Volcano\" href=\"http:\/\/www.avo.alaska.edu\/activity\/Pavlof.php#\"><strong>Pavlof Volcano<\/strong><\/a> began around 01:50 UTC on 13 November 2014. A comparison of nighttime images of Suomi NPP VIIRS 0.7 \u00b5m Day\/Night Band (DNB) and 3.74 \u00b5m shortwave IR data at 13:07 UTC or 4:07 am local time on 14 November <strong><em>(above)<\/em><\/strong> showed the bright glow of the eruption on the DNB image, with the hottest pixel being 52\u00ba C<em> (red color enhancement)<\/em> on the shortwave IR image.<\/p>\n<p>With the subsequent arrival of daylight, a break in the clouds allowed the faint volcanic plume to be observed on GOES-15 0.63 \u00b5m visible channel images <em><strong>(below; click image to play animation),<\/strong><\/em> drifting northwestward over the Bering Sea.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/11\/141114_goes15_visible_Pavlof_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/11\/141114_G15_VIS_PAVLOF_15.GIF\" alt=\"GOES-15 0.63 \u00b5m visible channel images (click to play animation)\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES-15 0.63 \u00b5m visible channel images (click to play animation)<\/p><\/div>\n<p>At 22:02 UTC on 14 November, the radiometrically-retrieved maximum volcanic ash mass loading value was 1.8 tons per km2, the maximum ash height was 16.8 km, and the maximum ash mass effective radius was 7.81 \u00b5m <em><strong>(below)<\/strong><\/em>.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/11\/141114_2202z_modis_ash_loading_ash_height_ash_effective_radius_Pavlof_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/11\/141114_2202z_modis_ash_loading_ash_height_ash_effective_radius_Pavlof_anim.gif\" alt=\"MODIS volcanic ash mass loading, ash height, and ash mass effective radius products\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">MODIS volcanic ash mass loading, ash height, and ash mass effective radius products<\/p><\/div>\n<p>About an hour later, the volcanic ash plume could be seen on a 23:03 UTC Suomi NPP VIIRS Day\/Night Band image, with a maximum 3.74 \u00b5m shortwave IR brightness temperature of 46\u00ba C at the summit of the volcano <em><strong>(below)<\/strong><\/em>.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/11\/141114_2303z_suomi_npp_viirs_dnb_swir_Pavlof_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/11\/141114_2303z_suomi_npp_viirs_dnb_swir_Pavlof_anim.gif\" alt=\"Suomi NPP VIIRS 0.7 \u00b5m Day\/Night Band and 3.74 \u00b5m shortwave IR images\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS 0.7 \u00b5m Day\/Night Band and 3.74 \u00b5m shortwave IR images<\/p><\/div>\n<p>The brown hue of the volcanic ash plume was very evident on Suomi NPP VIIRS true-color Red\/Green\/Blue (RGB) images from the <a title=\"SSEC RealEarth web map server\" href=\"http:\/\/wms.ssec.wisc.edu\"><strong>SSEC RealEarth<\/strong><\/a> web map server <em><strong>(below)<\/strong><\/em>.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/11\/141114_suomi_npp_viirs_truecolor_Pavlof_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/11\/141114_suomi_npp_viirs_truecolor_Pavlof_anim.gif\" alt=\"Suomi NPP VIIRS true-color RGB images\" width=\"480\" height=\"400\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS true-color RGB images<\/p><\/div>\n<p>The intensity of the Pavlof eruption increased on 15 November, and a well-defined volcanic ash plume could be seen on GOES-15 0.63 \u00b5m visible channel images<em><strong> (below; click image to play animation).<\/strong><\/em> Pilot reports estimated that the top of the plume was as high as 38,000 feet<em><strong>.<br \/>\n<\/strong><\/em><\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/11\/141115_goes15_visible_Pavlof_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/11\/141115_G15_VIS_PAVLOF_15.GIF\" alt=\"GOES-15 0.63 \u00b5m visible channel images (click to play animation)\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES-15 0.63 \u00b5m visible channel images (click to play animation)<\/p><\/div>\n<p>On a comparison of Suomi NPP VIIRS 0.64 \u00b5m visible channel and 11.45 \u00b5m IR channel images at 22:45 UTC<em><strong> (below),<\/strong><\/em> the coldest cloud-top IR brightness temperature value was -55\u00ba C.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/11\/141115_2244z_suomi_npp_viirs_visible_ir_Pavlof_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/11\/141115_2244z_suomi_npp_viirs_visible_ir_Pavlof_anim.gif\" alt=\"Suomi NPP VIIRS 0.64 \u00b5m visible channel and 11.45 \u00b5m IR channel images\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS 0.64 \u00b5m visible channel and 11.45 \u00b5m IR channel images<\/p><\/div>\n<p>At 22:29 UTC, the <a title=\"CLAVR -x\" href=\"http:\/\/cimss.ssec.wisc.edu\/clavr\/\"><strong>CLAVR-x<\/strong><\/a> POES AVHRR Cloud Top Temperature product indicated a minimum value of -54\u00ba C, with a maximum Cloud Top Height value of 9 km; the -54\u00ba C cloud top temperature corresponded to an altitude of around 29,000 feet or 8.7 km on the 16 November\/00 UTC <a title=\"Cold Bay AK rawinsonde profile\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/11\/PACB_20141116_0000.png\"><strong>Cold Bay AK rawinsonde profile<\/strong><\/a>.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/11\/141115_2229z_poes_avhrr_ctt_cth_Pavlof_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/11\/141115_2229z_poes_avhrr_ctt_cth_Pavlof_anim.gif\" alt=\"POES AVHRR Cloud Top Temperature and Cloud Top Height products\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">POES AVHRR Cloud Top Temperature and Cloud Top Height products<\/p><\/div>\n<p>A Suomi NPP VIIRS true-color RGB image at 23:04 UTC <em><strong>(below)<\/strong> <\/em>suggested that the volcanic plume consisted of a dense layer of tan-colored ash, with a layer of mostly ice cloud at the top of the plume.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/11\/141115_2304z_suomi_npp_viirs_truecolor_Pavlof.png\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/11\/141115_2304z_suomi_npp_viirs_truecolor_Pavlof.png\" alt=\"Suomi NPP VIIRS true-color RGB image\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS true-color RGB image<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>According to the Alaska Volcano Observatory, an eruption of the Pavlof Volcano began around 01:50 UTC on 13 November 2014. A comparison of nighttime images of Suomi NPP VIIRS 0.7 \u00b5m Day\/Night Band (DNB) and 3.74 \u00b5m shortwave IR data at 13:07 UTC or 4:07 am local time on 14 November (above) showed the bright [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":17182,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[22,43,12,26,53,45,49,48,9],"tags":[],"class_list":["post-17179","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-avhrr","category-goes-15","category-modis","category-poes","category-real-earth","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\/17179","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=17179"}],"version-history":[{"count":13,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/17179\/revisions"}],"predecessor-version":[{"id":17194,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/17179\/revisions\/17194"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/17182"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=17179"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=17179"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=17179"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}