{"id":48499,"date":"2022-10-26T18:09:14","date_gmt":"2022-10-26T18:09:14","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=48499"},"modified":"2022-10-31T17:02:11","modified_gmt":"2022-10-31T17:02:11","slug":"band-7-on-himawari-9-vs-band-7-on-himawari-8","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/48499","title":{"rendered":"Band 7 on Himawari-9 vs. Band 7 on Himawari-8"},"content":{"rendered":"\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/10\/HIMAWARI-8-9_AHI_convection_20221026_020019_FLDKGuamLogoTimetoggle.gif\"><img decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/10\/HIMAWARI-8-9_AHI_convection_20221026_020019_FLDKGuamLogoTimetoggle.gif\" alt=\"\" class=\"wp-image-48500\"\/><\/a><figcaption>Himawari-8 Visible Imagery (Band 3, 0.64 \u00b5m) along with Himawari-8 and Himawari-9 Day Convection RGB imagery, 0200 UTC on 26 October 2022, near Guam (click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>Himawari-9 is slated to become operational (replacing Himawari-8, which has been operational at 140.7<sup>o <\/sup>E Longitude since 2015!) on 13 December 2022 (<a href=\"https:\/\/space.oscar.wmo.int\/satellites\/view\/himawari_9\">Link<\/a>).  One change that users might observe arises from the slightly shorter central wavelength in the shortwave infrared band (Band 7).  On Himawari-8, the central wavelength is 3.885 \u00b5m;  on Himawari-9, the central wavelength is closer to 3.829 \u00b5m (see<a href=\"https:\/\/www.data.jma.go.jp\/mscweb\/en\/himawari89\/space_segment\/spsg_ahi.html\"> this link from JMA<\/a>, or <a href=\"https:\/\/www.data.jma.go.jp\/mscweb\/data\/monitoring\/gsics\/ir\/techinfo_geoleoir.html\">this one<\/a>).  The effect of the shorter wavelength on Himawari-9 is more noticeable during the daytime, when solar reflectance will lead to warmer observed brightness temperatures, especially over highly reflective convective updrafts (<a href=\"https:\/\/www.cira.colostate.edu\/wp-content\/uploads\/sites\/4\/2022\/10\/RGBworkshop_HANDA_TARO.pdf\">This presentation<\/a> &#8212; see slide 19 &#8212; given at the <a href=\"https:\/\/www.cira.colostate.edu\/conferences\/rgb_workshop\/\">CIRA RGB Workshop<\/a> in October 2022, suggests daytime differences of up to 5 C.), and especially when compared to longwave infrared imagery as a brightness temperature difference.<\/p>\n\n\n\n<p>The toggle above compares Himawari-8 visible imagery and <a href=\"https:\/\/www.star.nesdis.noaa.gov\/goes\/documents\/QuickGuide_GOESR_DayConvectionRGB_final.pdf\">Day Convection RGB<\/a> imagery from Himawari-8 and -9 at 0200 UTC on 26 October 2022. in a region near Guam, without much intense convection.  Subtle differences in the yellow shading over some convection are apparent (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/10\/HIMAWARI-8-9_AHI_day_convection_20221026_020019_FLDKGuamLogoTimetoggle.gif\">here&#8217;s a toggle<\/a> just between Himawari-8 and -9 Day Convection RGB over Guam).  It&#8217;s very hard to discern a difference in regions of no convection.<\/p>\n\n\n\n<p>For strong convection, however, as shown below for a case over the south-central Equatorial Pacific, differences in yellow coloring over very strong convection are noteable;  users might need to adjust the range of the RGB to draw out details in cloud tops, where, for Himawari-9 imagery, contrast is lost.  (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/10\/HIMAWARI-8_9_AHI_day_convection_20221026_020019_FLDKConvectionLogoTimetoggle.gif\">Here&#8217;s<\/a> a toggle, over the strong convection, between Day Convection RGBs from <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/10\/HIMAWARI-8_AHI_convection_20221026_020019_FLDKConvectionLogoTime.png\">Himawari-8<\/a> and <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/10\/HIMAWARI-9_AHI_convection_20221026_020019_FLDKConvectionLogoTime.png\">Himawari-9<\/a>).<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/10\/HIMAWARI-8-9_AHI_convection_20221026_020019_FLDKConvectionLogoTimetoggle.gif\" alt=\"\" class=\"wp-image-48503\"\/><figcaption>Himawari-8 Visible Imagery (Band 3, 0.64 \u00b5m) along with Himawari-8 and Himawari-9 Day Convection RGB imagery, 0200 UTC on 26 October 2022, over the Equatorial Pacific (click to enlarge)<\/figcaption><\/figure>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<p>Spectral Response Functions for the infrared channels are available from Himawari-8 (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/calibration\/SRF\/plots\/AHI08_SRFs_3panel_patches.png\">here<\/a>) and Himawari-9 (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/calibration\/SRF\/plots\/AHI09_SRFs_3panel_patches.png\">here<\/a>).  You will note that most infrared channels have similar functions;  the outlier is band 7, shown below (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/10\/AHI08_09_SRFs_Band07_toggle.gif\">and in this animated gif<\/a>).<\/p>\n\n\n<div\n\t\tclass=\"ssec_slider_juxtapose\"\n\t\tid=\"ssec_slider_juxtapose_562855001\"\n\t\tdata-left-src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/10\/AHI08_SRFs_Band07LL.png\"\n\t\tdata-left-label=\"Himawari-8 Spectral Response Function, shortwave IR, Band 7\"\n\t\tdata-right-src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/10\/AHI09_SRFs_Band07LL.png\"\n\t\tdata-right-label=\"Himawari-9 Spectral Response Function, shortwave IR, Band 7\"\n\t\tdata-width=\"630\"\n\t\tdata-height=\"340\"\n\t\tdata-left-orig-src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/10\/AHI08_SRFs_Band07LL.png\"\n\t\tdata-right-orig-src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/10\/AHI09_SRFs_Band07LL.png\">\n\t<span class=\"ssec_slider_juxtapose_fullscreen_button\">\n\t\t<span class=\"fullscreen-icon\"><svg viewBox=\"0 0 12 12\" preserveAspectRatio=\"xMidYMid\" tabindex=\"-1\">\n\t\t\t<polyline class=\"fill\" points=\"6,6 5.9,2 4.9,3 2.9,1 1,2.9 3,4.9 2,5.9\"\n\t\t\t\t\t  transform=\"translate(6,6)\"><\/polyline>\n\t\t\t<polyline class=\"fill\" points=\"6,6 5.9,2 4.9,3 2.9,1 1,2.9 3,4.9 2,5.9\"\n\t\t\t\t\t  transform=\"translate(6,6) rotate(90)\"><\/polyline>\n\t\t\t<polyline class=\"fill\" points=\"6,6 5.9,2 4.9,3 2.9,1 1,2.9 3,4.9 2,5.9\"\n\t\t\t\t\t  transform=\"translate(6,6) rotate(180)\"><\/polyline>\n\t\t\t<polyline class=\"fill\" points=\"6,6 5.9,2 4.9,3 2.9,1 1,2.9 3,4.9 2,5.9\"\n\t\t\t\t\t  transform=\"translate(6,6) rotate(270)\"><\/polyline>\n\t\t\t<\/svg>\n\t\t<\/span>\n\t<\/span>\n<\/div>\n\n\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<p>Thanks to <a href=\"https:\/\/www.jma.go.jp\/jma\/indexe.html\">JMA<\/a> for providing simultaneous image files for the different bands on Himawari-8 and Himawari-9!<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Himawari-9 is slated to become operational (replacing Himawari-8, which has been operational at 140.7o E Longitude since 2015!) on 13 December 2022 (Link). One change that users might observe arises from the slightly shorter central wavelength in the shortwave infrared band (Band 7). On Himawari-8, the central wavelength is 3.885 \u00b5m; on Himawari-9, the central [&hellip;]<\/p>\n","protected":false},"author":19,"featured_media":48505,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[62,73,45],"tags":[],"class_list":["post-48499","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-himawari-8","category-himawari-9","category-redgreenblue-rgb-images"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/48499","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=48499"}],"version-history":[{"count":6,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/48499\/revisions"}],"predecessor-version":[{"id":48564,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/48499\/revisions\/48564"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/48505"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=48499"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=48499"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=48499"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}