{"id":12453,"date":"2013-03-07T23:59:48","date_gmt":"2013-03-07T23:59:48","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=12453"},"modified":"2013-03-08T16:51:51","modified_gmt":"2013-03-08T16:51:51","slug":"volcanic-ash-fall-plume-over-the-kamchatka-peninsula","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/12453","title":{"rendered":"Volcanic ash fall plume over the Kamchatka Peninsula"},"content":{"rendered":"<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/03\/130307_suomi_npp_viirs_vis_kamchatka_anim.gif\"><img loading=\"lazy\" decoding=\"async\" alt=\"Suomi NPP VIIRS 0.64 \u00c2\u00b5m visible channel images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/03\/130307_suomi_npp_viirs_vis_kamchatka_anim.gif\" width=\"480\" height=\"380\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS 0.64 \u00c2\u00b5m visible channel images<\/p><\/div>\n<p>AWIPS images of Suomi NPP VIIRS 0.64 \u00c2\u00b5m visible channel images <strong><em>(above)<\/em><\/strong> revealed some interesting curved ice floe gyres in the Bering Sea just off the eastern coast of the Russian Kamchatka Peninsula on <strong>07 March 2013<\/strong>. Also evident near the center of the visible images was a long, narrow, and slightly darker feature that was oriented approximately west-to-east, and located to the northwest and north of the village of Ust&#8217;-Kamchatsk <em>(station identifier 32408)<\/em>. This darker feature was a volcanic ash fall plume from the <strong><a title=\"Sheveluch Volcano\" href=\"http:\/\/www.volcanodiscovery.com\/kamchatka\/sheveluch\/news.html\">Sheveluch Volcano<\/a><\/strong> <em>(located 31 miles or 50 km to the northwest),<\/em> which had experienced eruptions\u00c2\u00a0producing volcanic ash\u00c2\u00a0(<a title=\"photos of Sheveluch volcanic eruption activity\" href=\"http:\/\/www.kscnet.ru\/ivs\/kvert\/current_eng.php?name=Sheveluch\"><strong>photos<\/strong><\/a>) on <strong><a title=\"02 March Sheveluch volcano ash advisory\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/03\/130302_sheveluch_vaa.text\">02 March<\/a><\/strong> and <strong><a title=\"04 March Sheveluch volcano ash advisory\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/03\/130304_sheveluch_vaa.text\">04 March<\/a><\/strong>  &#8212; the darker color of the narrow strip of volcanic ash made it stand out against the adjacent snow-covered areas (<a title=\"annotated visible image\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/03\/VIIRS_0.64_REF_20130307_0206_anotated.png\"><strong>annotated visible image<\/strong><\/a>).<\/p>\n<p>A comparison of a Suomi NPP VIIRS 0.64 \u00c2\u00b5m visible channel image with the corresponding false-color Red\/Green\/Blue (RGB) image <strong><em>(below)<\/em><\/strong> also showed the contrast between the narrow strip of ash-covered snow and the surrounding undisturbed snow cover <em>(snow and ice appear as darker shades of red in the RGB image)<\/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\/2013\/03\/130307_0206z_suomi_npp_viirs_vis_rgb_kamchatka_anim.gif\"><img loading=\"lazy\" decoding=\"async\" alt=\"Suomi NPP VIIRS 0.64 \u00c2\u00b5m visible channel image + False-color Red\/Green\/Blue (RGB) image\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/03\/130307_0206z_suomi_npp_viirs_vis_rgb_kamchatka_anim.gif\" width=\"480\" height=\"380\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS 0.64 \u00c2\u00b5m visible channel image + False-color Red\/Green\/Blue (RGB) image<\/p><\/div>\n<p>A comparison of Suomi NPP VIIRS 0.64 \u00c2\u00b5m visible channel, 3.74 \u00c2\u00b5m shortwave IR channel, and 11.45 \u00c2\u00b5m IR channel images <strong><em>(below)<\/em><\/strong> showed that the strip of ash-covered snow appeared significantly warmer <em>(darker)<\/em> on the shortwave IR image, due to the fact that the volcanic ash particles were efficient reflectors of incoming solar radiation. The ash-covered snow even appeared slightly warmer <em>(darker)<\/em> on the 11.45 \u00c2\u00b5m IR image, since the lower albedo of the ash-covered snow allowed it to absorb more incoming solar radiation.Also evident on the shortwave IR image was a distinct hot thermal anomaly <em>(yellow to red color enhancement)<\/em> associated with the active Kizimen volcano.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/03\/130307_0206z_suomi_npp_viirs_vis_swir_ir_kamchatka_anim.gif\"><img loading=\"lazy\" decoding=\"async\" alt=\"Suomi NPP VIIRS 0.64 \u00c2\u00b5m visible channel, 3.74 \u00c2\u00b5m shortwave IR channel. and 11.45 \u00c2\u00b5m IR channel images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/03\/130307_0206z_suomi_npp_viirs_vis_swir_ir_kamchatka_anim.gif\" width=\"480\" height=\"380\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS 0.64 \u00c2\u00b5m visible channel, 3.74 \u00c2\u00b5m shortwave IR channel. and 11.45 \u00c2\u00b5m IR channel images<\/p><\/div>\n<p>An animation of McIDAS images of MTSAT-2 0.73 \u00c2\u00b5m visible channel data <strong><em>(below; click image to play animation)<\/em><\/strong> confirmed that the darker volcanic ash fall plume was a stationary feature, and not an airborne volcanic ash plume. The animation also showed the anticyclonic rotation of the gyres of ice floes just off the east coast of Kamchatka.<\/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\/2013\/03\/130306-07_mtsat_vis_kamchatka_ash_fall_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\" \" title=\"MTSAT-2 0.73 \u00c2\u00b5m visible channel images (click image to play animation)\" alt=\"MTSAT-2 0.73 \u00c2\u00b5m visible channel images (click image to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/03\/130306-07_MTSAT_VIS_KAMCHATKA_ASH_FALL_08.GIF\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">MTSAT-2 0.73 \u00c2\u00b5m visible channel images (click image to play animation)<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>AWIPS images of Suomi NPP VIIRS 0.64 \u00c2\u00b5m visible channel images (above) revealed some interesting curved ice floe gyres in the Bering Sea just off the eastern coast of the Russian Kamchatka Peninsula on 07 March 2013. Also evident near the center of the visible images was a long, narrow, and slightly darker feature that [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[37,20,45,49,48,9],"tags":[],"class_list":["post-12453","post","type-post","status-publish","format-standard","hentry","category-arctic","category-mtsat","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\/12453","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=12453"}],"version-history":[{"count":9,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/12453\/revisions"}],"predecessor-version":[{"id":12458,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/12453\/revisions\/12458"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=12453"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=12453"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=12453"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}