{"id":17344,"date":"2014-12-18T15:34:49","date_gmt":"2014-12-18T15:34:49","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=17344"},"modified":"2014-12-22T19:42:18","modified_gmt":"2014-12-22T19:42:18","slug":"himawari-8-is-broadcasting-data","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/17344","title":{"rendered":"First images from Himawari-8"},"content":{"rendered":"<div style=\"width: 430px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/www.jma-net.go.jp\/sat\/data\/web89\/parts89\/himawari8_first_image\/grs_m\/B03_m.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/12\/B03_m.jpg\" alt=\"Himawari-8 0.64 \u00b5m visible channel image (click to enlage)\" width=\"420\" height=\"430\" \/><\/a><p class=\"wp-caption-text\">Himawari-8 0.64 \u00b5m visible channel image (click to enlarge)<\/p><\/div>\n<p>The <a href=\"http:\/\/www.jma.go.jp\/jma\/indexe.html\">Japan Meteorological Agency<\/a> has released the first images from the <a title=\"AHI\" href=\"http:\/\/www.data.jma.go.jp\/mscweb\/en\/himawari89\/space_segment\/spsg_ahi.html\">AHI<\/a> instrument on the Himawari-8 satellite, which was launched on <a title=\"07 October 2014 Himawari-8 launch \" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/16830\">7 October<\/a> this year.<\/p>\n<p><a href=\"http:\/\/www.jma.go.jp\/jma\/jma-eng\/satellite\/news\/himawari89\/20141218_himawari8_first_images.html\">This link<\/a> shows full disk imagery from all 16 spectral bands. The AHI on Himawari-8 is very similar to the <a title=\"ABI\" href=\"http:\/\/www.goes-r.gov\/spacesegment\/abi.html\">ABI<\/a> that will fly on GOES-R.<\/p>\n<p>A comparison of images using each of the 16 spectral bands is shown below, centered over the Sea of Japan. Cloud streets are seen over much of the open waters, due to the southeastward and eastward transport of very cold air from Siberia (<a title=\"water vapor image with surface analysis\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/12\/N_Pac_Sfc_Anal_20141218_0600.png\">surface analysis<\/a>). Lee waves (or &#8220;mountain waves&#8221;) are evident on the water vapor bands (8, 9\u00a0 and 10) downwind or southeast of the higher terrain areas on the main Japanese island of Honshu.<\/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\/12\/141218_0240z_himiwari8_Japan_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/12\/141218_0240z_himiwari8_Japan_anim.gif\" alt=\"Comparison of the 16 AHI spectral bands, centered on the Sea of Japan (click to enlarge)\" width=\"480\" height=\"400\" \/><\/a><p class=\"wp-caption-text\">Comparison of the 16 AHI spectral bands, centered on the Sea of Japan (click to enlarge)<\/p><\/div>\n<table border=\"1\">\n<tbody>\n<tr>\n<th>\u00a0Band<\/th>\n<th><i><span style=\"color: darkgreen;\"> 1<\/span><\/i><\/th>\n<th><i><span style=\"color: darkgreen;\"> 2<\/span><\/i><\/th>\n<th><i><span style=\"color: darkgreen;\"> 3<\/span><\/i><\/th>\n<th><span style=\"color: green;\"> 4<\/span><\/th>\n<th><span style=\"color: green;\"> 5<\/span><\/th>\n<th><span style=\"color: green;\"> 6<\/span><\/th>\n<th><span style=\"color: blue;\"> 7<\/span><\/th>\n<th><span style=\"color: blue;\"> 8<\/span><\/th>\n<th><span style=\"color: blue;\"> 9<\/span><\/th>\n<th><span style=\"color: blue;\"> 10<\/span><\/th>\n<th><span style=\"color: blue;\"> 11<\/span><\/th>\n<th><span style=\"color: blue;\"> 12<\/span><\/th>\n<th><span style=\"color: blue;\"> 13<\/span><\/th>\n<th><span style=\"color: blue;\"> 14<\/span><\/th>\n<th><span style=\"color: blue;\"> 15<\/span><\/th>\n<th><span style=\"color: blue;\"> 16<\/span><\/th>\n<\/tr>\n<tr>\n<th>\u00b5m<\/th>\n<th><i><span style=\"color: darkgreen;\">\u00a00.47\u00a0<\/span><\/i><\/th>\n<th><i><span style=\"color: darkgreen;\">\u00a00.52\u00a0<\/span><\/i><\/th>\n<th><i><span style=\"color: darkgreen;\">\u00a00.64\u00a0<\/span><\/i><\/th>\n<th><span style=\"color: green;\">\u00a00.86\u00a0<\/span><\/th>\n<th><span style=\"color: green;\">\u00a01.6\u00a0<\/span><\/th>\n<th><span style=\"color: green;\">\u00a02.3\u00a0<\/span><\/th>\n<th><span style=\"color: blue;\">\u00a03.9\u00a0<\/span><\/th>\n<th><span style=\"color: blue;\">\u00a06.2\u00a0<\/span><\/th>\n<th><span style=\"color: blue;\">\u00a06.9\u00a0<\/span><\/th>\n<th><span style=\"color: blue;\">\u00a07.3\u00a0<\/span><\/th>\n<th><span style=\"color: blue;\">\u00a08.6\u00a0<\/span><\/th>\n<th><span style=\"color: blue;\">\u00a09.6\u00a0<\/span><\/th>\n<th><span style=\"color: blue;\">\u00a010.4\u00a0<\/span><\/th>\n<th><span style=\"color: blue;\">\u00a011.2\u00a0<\/span><\/th>\n<th><span style=\"color: blue;\">\u00a012.4\u00a0<\/span><\/th>\n<th><span style=\"color: blue;\">\u00a013.3\u00a0<\/span><\/th>\n<\/tr>\n<\/tbody>\n<\/table>\n<p>Similar comparisons of Himawari-8 images covering Hawaii, western Australia, and the far Southern Hemisphere are available on the <a title=\"First Light AHI Satellite Band Webapp\" href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/webapps\/bandapp\/overview_ahi_first_light.html\">First Light AHI Satellite Band Webapp<\/a>.<\/p>\n<p>As seen on the MTSAT-2 vs Himawari-8 comparison below, even at large satellite viewing angles over the far southern portion of the Southern Hemisphere (for example, <a title=\"MTSAT-2 water vapor image with map overlay\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/12\/141218_0232Z_MTSAT2_WV_SH_LARGE.GIF\">between Australia\/Tasmania and Antarctica<\/a>) AHI imagery such as that from water vapor channels exhibits higher quality (due to factors such as improved spatial resolution, signal-to-noise ratio, data bit depth, etc).<\/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\/12\/141218_0230z_mtsat_himawari_water_vapor_SH.png\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/12\/141218_0230z_mtsat_himawari_water_vapor_SH.png\" alt=\"MTSAT-2 vs Himawari-8 water vapor channel images\" width=\"480\" height=\"130\" \/><\/a><p class=\"wp-caption-text\">MTSAT-2 vs Himawari-8 water vapor channel images<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>The Japan Meteorological Agency has released the first images from the AHI instrument on the Himawari-8 satellite, which was launched on 7 October this year. This link shows full disk imagery from all 16 spectral bands. The AHI on Himawari-8 is very similar to the ABI that will fly on GOES-R. A comparison of images [&hellip;]<\/p>\n","protected":false},"author":19,"featured_media":17357,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[34,62,20],"tags":[],"class_list":["post-17344","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-r","category-himawari-8","category-mtsat"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/17344","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=17344"}],"version-history":[{"count":43,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/17344\/revisions"}],"predecessor-version":[{"id":17410,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/17344\/revisions\/17410"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/17357"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=17344"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=17344"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=17344"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}