{"id":42700,"date":"2021-10-01T13:33:28","date_gmt":"2021-10-01T13:33:28","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=42700"},"modified":"2021-10-01T16:01:23","modified_gmt":"2021-10-01T16:01:23","slug":"kilauea-is-active-again","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/42700","title":{"rendered":"Kilauea is active again"},"content":{"rendered":"\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/10\/G17Band7-20211001_0126_to_1156anim.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"1353\" height=\"1022\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/10\/G17Band7-20211001_0126_to_1156anim.gif\" alt=\"\" class=\"wp-image-42701\" \/><\/a><figcaption>GOES-17 Shortwave Infrared, 0126 &#8211; 1156 UTC on 1 October 2021 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>GOES-17 Shortwave Infrared imagery, above, shows the hot-spot associated with the latest eruptive phase of the Halema&#8217;uma&#8217;u Crater on Kilauea&#8217;s southern slope. (Click <a href=\"https:\/\/www.usgs.gov\/volcanoes\/kilauea\/summit-webcams\">here<\/a> for webcams).<\/p>\n\n\n\n<p>The Day Night band from VIIRS on board Suomi NPP and NOAA-20 show the light source from the eruption as well, as shown in the toggle below (imagery from the Honolulu Direct Broadcast site, <a href=\"http:\/\/soest-hcc1.hcc.hawaii.edu\/browser\/\">here<\/a>)<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/10\/viirs_adaptive_dnb_20211001_1111_1200_HONOLULUtoggle.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"1024\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/10\/viirs_adaptive_dnb_20211001_1111_1200_HONOLULUtoggle.gif\" alt=\"\" class=\"wp-image-42702\" \/><\/a><figcaption>VIIRS Day Night Band imagery from Suomi NPP (1111 UTC) and NOAA-20 (1200 UTC), 1 October 2021 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>The NOAA\/CIMSS Volcanic Cloud Monitoring Web Portal (<em>i.e.<\/em>, VOLCAT &#8212; <a href=\"https:\/\/volcano.ssec.wisc.edu\/\">link<\/a>) include a Kilauea sector under the Washington DC VAAC tab;  an imagery example is <a href=\"https:\/\/volcano.ssec.wisc.edu\/imagery\/view\/#sector:Kilauea_250_m::instr:ABI::sat:all::image_type:RGB1112or13um_3911um_11um::endtime:2021-10-01_12-21-30::daterange:240\">here<\/a>.<\/p>\n\n\n\n<hr class=\"wp-block-separator\" \/>\n\n\n\n<p>FDCA &#8212; the Fire Detection and Characterization Algorithm &#8212; should have a signal here but does not.  The landcover dataset used for the product is <em><strong>missing Hawaii<\/strong><\/em>.  Fires aren&#8217;t looked for when land does not exist, even if its absence is in error.  NOAA\/NESDIS Scientists and their partners at <a href=\"https:\/\/cimss.ssec.wisc.edu\">CIMSS<\/a> are working to correct this oversight.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>GOES-17 Shortwave Infrared imagery, above, shows the hot-spot associated with the latest eruptive phase of the Halema&#8217;uma&#8217;u Crater on Kilauea&#8217;s southern slope. (Click here for webcams). The Day Night band from VIIRS on board Suomi NPP and NOAA-20 show the light source from the eruption as well, as shown in the toggle below (imagery from [&hellip;]<\/p>\n","protected":false},"author":19,"featured_media":42704,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[80,78,49,48,9],"tags":[],"class_list":["post-42700","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-17","category-noaa-20","category-suomi_npp","category-viirs","category-volcanic-activity"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/42700","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\/19"}],"replies":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/comments?post=42700"}],"version-history":[{"count":4,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/42700\/revisions"}],"predecessor-version":[{"id":42708,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/42700\/revisions\/42708"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/42704"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=42700"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=42700"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=42700"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}