{"id":24542,"date":"2017-07-21T23:59:44","date_gmt":"2017-07-21T23:59:44","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=24542"},"modified":"2017-07-22T17:30:10","modified_gmt":"2017-07-22T17:30:10","slug":"goes-16-glm-data-now-available-in-realearth","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/24542","title":{"rendered":"GOES-16 GLM data now available in RealEarth\u2122"},"content":{"rendered":"<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2017\/07\/170721_2030_2200_goes16_mesoscale_infrared_glm_Iowa_City_IA_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2017\/07\/170721_2200utc_goes16_infrared_glm_Iowa_City_IA.png\" alt=\"GOES-16 Infrared Window (103 \u00b5m) images, with GLM Group data points plotted as white dots [click to play animation]\" width=\"640\" height=\"417\" \/><\/a><p class=\"wp-caption-text\">GOES-16 Infrared Window (10.3 \u00b5m) images, with GLM Group data points plotted as white dots [click to play animation]<\/p><\/div><em>* GOES-16 data posted on this page are preliminary, non-operational and are undergoing testing *<\/em><\/p>\n<p>Real-time GOES-16 Geostationary Lightning Mapper (<a href=\"http:\/\/www.goes-r.gov\/spacesegment\/glm.html\"><strong>GLM<\/strong><\/a>) data are now available for viewing using <a href=\"http:\/\/realearth.ssec.wisc.edu\"><strong>RealEarth<\/strong><\/a>\u2122 (real-time <a href=\"https:\/\/re.ssec.wisc.edu\/s\/Px6TM\"><strong>GLM link<\/strong><\/a>). An example from 21 July 2017 is shown above, for an isolated\u00a0thunderstorm that developed during the afternoon hours along a residual convective outflow boundary &#8212; which was evident on an <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2017\/07\/170721_goes16_visible_IA_anim.gif\"><strong>animation<\/strong><\/a> of &#8220;Red&#8221; Visible (<a href=\"http:\/\/www.goes-r.gov\/education\/docs\/ABI-bands-FS\/ABI%20Fact%20Sheet%20Band%202.pdf\"><strong>0.64 \u00b5m<\/strong><\/a>) imagery &#8212; draped across eastern Iowa. This storm produced 1.0-inch diameter hail and damaging winds within 7-22 minutes after the 2200 UTC end of the animation (<a href=\"http:\/\/www.spc.noaa.gov\/climo\/reports\/170721_rpts.html\"><strong>SPC storm reports<\/strong><\/a>).\u00a0 Both the GOES-16 &#8220;Clean&#8221; Infrared Window <a href=\"http:\/\/www.goes-r.gov\/education\/docs\/ABI-bands-FS\/ABI_Band_13_FS_CLEAN_LW_IR_FINAL.pdf\"><strong>(10.3 \u00b5m<\/strong><\/a>) images and the GLM <em>Group<\/em> (GLM <em>Events<\/em> clustered by proximity; see <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/24440\"><strong>this<\/strong><\/a> blog post) data points were available at 1-minute intervals, since the region was within the domain of one of the <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/23225\"><strong>Mesoscale Sectors<\/strong><\/a>.<\/p>\n<p>Note that during the early portion of the animation, a number of GLM Group points were located south of the rapidly-expanding cold cloud top shield &#8212; GLM data are <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/217\"><strong>parallax<\/strong><\/a>-corrected, assuming a cloud-top height of 12.5 km. The 18 UTC tropopause height was 15.0 km on the <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2017\/07\/170721_18UTC_DVN_RAOB.GIF\"><strong>18 UTC sounding<\/strong><\/a> at Davenport, Iowa.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>* GOES-16 data posted on this page are preliminary, non-operational and are undergoing testing * Real-time GOES-16 Geostationary Lightning Mapper (GLM) data are now available for viewing using RealEarth\u2122 (real-time GLM link). An example from 21 July 2017 is shown above, for an isolated\u00a0thunderstorm that developed during the afternoon hours along a residual convective outflow [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":24544,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[76,74,30],"tags":[],"class_list":["post-24542","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-glm","category-goes-16","category-lightning"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/24542","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=24542"}],"version-history":[{"count":23,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/24542\/revisions"}],"predecessor-version":[{"id":24566,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/24542\/revisions\/24566"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/24544"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=24542"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=24542"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=24542"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}