{"id":13992,"date":"2013-09-22T23:59:11","date_gmt":"2013-09-22T23:59:11","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=13992"},"modified":"2013-10-01T19:37:22","modified_gmt":"2013-10-01T19:37:22","slug":"resuspended-ash-from-the-katmai-volcano-in-alaska","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/13992","title":{"rendered":"Re-suspended ash from the Katmai volcano in Alaska"},"content":{"rendered":"<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\/09\/130922_g15_vis_katmai_ash_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"GOES-15 0.63 \u00c2\u00b5m visible channel images (click image to play animation)\" alt=\"GOES-15 0.63 \u00c2\u00b5m visible channel images (click image to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/09\/130922_G15_VIS_KATMAI_ASH_14.GIF\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES-15 0.63 \u00c2\u00b5m visible channel images (click image to play animation)<\/p><\/div>\n<p>GOES-15 0.63 \u00c2\u00b5m visible channel images <em><strong>(above; click image to play animation)<\/strong><\/em> showed a distinct hazy plume streaming southeastward from the Katmai volcano area in Alaska on 22 September 2013. This was a signature of re-suspended volcanic ash &#8212; a deep layer of ash has remained on the ground near the volcano following the massive <a title=\"Katmai volcano (Volcano Discovery)\" href=\"http:\/\/www.volcanodiscovery.com\/katmai.html\"><strong>1912 eruption<\/strong><\/a> &#8212; which was carried aloft by strong winds on the back side of a deep area of low pressure over the Gulf of Alaska <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\/2013\/09\/VIIRS_DNB_N_Pac_Sfc_Anal_20130923_0000.png\"><img loading=\"lazy\" decoding=\"async\" title=\"Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band image\" alt=\"Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band image\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/09\/VIIRS_DNB_N_Pac_Sfc_Anal_20130923_0000.png\" width=\"480\" height=\"296\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band image<\/p><\/div>\n<p>A closer view using a sequence of four Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band images <em><strong>(below)<\/strong><\/em> showed the evolution of the ash plume as it moved over southeastward over Kodiak Island and then out over the Gulf of Alaska. Winds at Kodiak <em>(station identifier PADQ)<\/em> gusted as high as 55 knots or 63 mph. With limited snow cover and strong winds <em>(which were enhanced by local terrain effects),<\/em> the surface volcanic ash was easily lofted to great heights.<\/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\/09\/130922_suomi_npp_viirs_dnb_ash_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band images\" alt=\"Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/09\/130922_suomi_npp_viirs_dnb_ash_AK_anim.gif\" width=\"480\" height=\"350\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band images<\/p><\/div>\n<p>An image of a MODIS-based NOAA\/STAR\/CIMSS Volcanic Ash Height product is shown in combination with the Volcanic Ash Advisory that was issued by the Anchorage Volcanic Ash Advisory Center <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\/2013\/09\/130922_katmai_modis_ash_height_ash_advisory.jpg\"><img loading=\"lazy\" decoding=\"async\" title=\"MODIS Ash Height product with Volcanic Ash Advisory\" alt=\"MODIS Ash Height product with Volcanic Ash Advisory\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/09\/130922_katmai_modis_ash_height_ash_advisory.jpg\" width=\"480\" height=\"351\" \/><\/a><p class=\"wp-caption-text\">MODIS Ash Height product with Volcanic Ash Advisory<\/p><\/div>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/09\/130922_modis_ash_height_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"MODIS Ash Height product\" alt=\"MODIS Ash Height product\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/09\/130922_modis_ash_height_AK_anim.gif\" width=\"480\" height=\"350\" \/><\/a><p class=\"wp-caption-text\">MODIS Ash Height product<\/p><\/div>\n<p>A sequence of three MODIS Volcanic Ash Height product images<em><strong> (above)<\/strong><\/em> suggested that the average height of the re-suspended ash plume was around 9,000 &#8211; 11,000 feet. A vertical profile of <a title=\"CALIPSO\" href=\"http:\/\/www-calipso.larc.nasa.gov\/\"><strong>CALIPSO<\/strong><\/a> satellite-based lidar data near the source of the ash plume <em><strong>(below; courtesy of Mike Pavolonis, NOAA\/NESDIS\/STAR)<\/strong><\/em> indicated that the top of the plume was around 3.5 km or 11,000 feet (at 12:57 UTC, near latitude\/longitude 58 N \/ 155 W).<\/p>\n<div style=\"width: 489px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/09\/130922_calipso_backscatter_katmai_plume.png\"><img loading=\"lazy\" decoding=\"async\" title=\"CALIPSO total attenuated backscatter\" alt=\"CALIPSO total attenuated backscatter\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/09\/130922_calipso_backscatter_katmai_plume.png\" width=\"479\" height=\"156\" \/><\/a><p class=\"wp-caption-text\">CALIPSO total attenuated backscatter<\/p><\/div>\n<p>The corresponding MODIS Ash Mass Loading product <em><strong>(below)<\/strong><\/em> indicated values of 2-3 tons per square kilometer existed over much of the ash 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\/2013\/09\/130922_modis_ash_mass_loading_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"MODIS Ash Mass Loading product\" alt=\"MODIS Ash Mass Loading product\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/09\/130922_modis_ash_mass_loading_AK_anim.gif\" width=\"480\" height=\"350\" \/><\/a><p class=\"wp-caption-text\">MODIS Ash Mass Loading product<\/p><\/div>\n<p>Finally, the corresponding MODIS Ash Mass Effective Radius product <em><strong>(below)<\/strong><\/em> showed that much of the plume likely consisted of particles with radii in the 4-6 \u00c2\u00b5m range, with a maximum value of 8.33 \u00c2\u00b5m.<\/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\/09\/130922_modis_ash_eff_radius_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"MODIS Ash Mass Effective Radius product\" alt=\"MODIS Ash Mass Effective Radius product\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/09\/130922_modis_ash_eff_radius_AK_anim.gif\" width=\"480\" height=\"350\" \/><\/a><p class=\"wp-caption-text\">MODIS Ash Mass Effective Radius product<\/p><\/div>\n<p style=\"text-align: left;\">Additional information on the NOAA\/UW-CIMSS GOES-R Volcanic Ash Products shown above can be found in this Java-based <a title=\"VISITview lesson\" href=\"http:\/\/www.ssec.wisc.edu\/visit\/lessons\/volash\/viewit.html\"><strong>VISITview lesson<\/strong><\/a> <em>(a separate Lesson Playback Control window will open to assist in viewing the lesson content)<\/em>.<\/p>\n<p style=\"text-align: center;\"><strong>===== 23 September Update =====<\/strong><\/p>\n<div style=\"width: 489px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/09\/VIIRS_DNB__REF_20130923_2136.png\"><img loading=\"lazy\" decoding=\"async\" title=\"Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band image\" alt=\"Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band image\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/09\/VIIRS_DNB__REF_20130923_2136.png\" width=\"479\" height=\"296\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band image<\/p><\/div>\n<p>On the following day <em>(23 September),<\/em> a Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band image <em><strong>(above)<\/strong><\/em> showed that the resuspended Katmai ash plume was still present, but was much less expansive than what was seen on 22 September.<\/p>\n<p>Hat tip to Mark Ruminski of the NOAA\/NESDIS Satellite Services Division for bringing this interesting event to our attention!<\/p>\n","protected":false},"excerpt":{"rendered":"<p>GOES-15 0.63 \u00c2\u00b5m visible channel images (above; click image to play animation) showed a distinct hazy plume streaming southeastward from the Katmai volcano area in Alaska on 22 September 2013. This was a signature of re-suspended volcanic ash &#8212; a deep layer of ash has remained on the ground near the volcano following the massive [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":14051,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[37,21,43,34,12,47,49,48,9],"tags":[],"class_list":["post-13992","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-arctic","category-aviation","category-goes-15","category-goes-r","category-modis","category-other-satellites","category-suomi_npp","category-viirs","category-volcanic-activity"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/13992","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=13992"}],"version-history":[{"count":18,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/13992\/revisions"}],"predecessor-version":[{"id":14031,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/13992\/revisions\/14031"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/14051"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=13992"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=13992"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=13992"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}