{"id":31922,"date":"2019-02-19T19:01:36","date_gmt":"2019-02-19T19:01:36","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=31922"},"modified":"2019-02-20T21:18:53","modified_gmt":"2019-02-20T21:18:53","slug":"testing-of-goes-16-and-goes-17-mode-6-scan-strategy","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/31922","title":{"rendered":"Testing of GOES-16 and GOES-17 Mode 6 scan strategy"},"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\/2019\/02\/190219_goes16_visible_Full_Disk_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/02\/G16_FD_VIS_B2_19FEB2019_2019050_163016_GOES-16_0001PANEL.GIF\" alt=\"GOES-16 \" width=\"640\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">GOES-16 &#8220;Red&#8221; Visible <em>(0.64 \u00b5m)<\/em> images [click to play animation]<\/p><\/div>Both GOES-16 <em>(GOES-East)<\/em> and GOES-17<em> (GOES-West)<\/em> were placed into the <strong>Mode 6<\/strong> scan strategy for a 3-day period of testing beginning at 1500 UTC on 19\u00a0 February 2019 &#8212; which provides Full Disk images every 10 minutes (instead of every 15 minutes for the more common Mode 3 scan strategy). Further details on GOES-R series scan modes are available <a href=\"https:\/\/journals.ametsoc.org\/doi\/full\/10.1175\/BAMS-D-15-00230.1\"><strong>here<\/strong><\/a> and <a href=\"https:\/\/satelliteliaisonblog.com\/2018\/11\/27\/goes-17-abi-mode-6-test\/\"><strong>here<\/strong><\/a>. GOES-16 Full Disk &#8220;Red&#8221; Visible (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band02.pdf\"><strong>0.64 \u00b5m<\/strong><\/a>) images are shown above, with Mid-level Water Vapor (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band09.pdf\"><strong>6.9 \u00b5m<\/strong><\/a>) images below.<\/p>\n<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\/2019\/02\/190219_goes16_waterVapor_Full_Disk_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/02\/G16_FD_WV_B9_19FEB2019_2019050_163016_GOES-16_0001PANEL.GIF\" alt=\"GOES-16 Mid-level Water Vapor (6.9 \u00b5m) images [click to play animation]\" width=\"640\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">GOES-16 Mid-level Water Vapor<em> (6.9 \u00b5m)<\/em> images [click to play animation]<\/p><\/div>One of the more striking features over the North Atlantic Ocean was a rapidly-intensifying <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/02\/190219_12utc_afc_Atlantic.png\"><strong>Hurricane Force low<\/strong><\/a> &#8212; an animation that cycles through GOES-16 Visible and Water Vapor images of this system is displayed below.<\/p>\n<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\/2019\/02\/190219_goes16_visible_waterVapor_Atlantic_low_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/02\/G16_ATL_LOW_WV_B9_19FEB2019_2019050_163016_GOES-16_0001PANEL.GIF\" alt=\"GOES-16 &quot;Red&quot; Visible (0.64 \u00b5m) and Mid-level Water Vapor (6.9 \u00b5m) images [click to play animation]\" width=\"640\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">GOES-16 &#8220;Red&#8221; Visible<em> (0.64 \u00b5m)<\/em> and Mid-level Water Vapor<em> (6.9 \u00b5m)<\/em> images [click to play animation]<\/p><\/div>GOES-16 <a href=\"http:\/\/rammb.cira.colostate.edu\/training\/visit\/quick_guides\/QuickGuide_GOESR_AirMassRGB_final.pdf\"><strong>Air Mass RGB<\/strong><\/a> images from the <a href=\"http:\/\/www.aos.wisc.edu\/weather\/wx_obs\/GOES16.html\"><strong>AOS<\/strong><\/a> site <em><strong>(below)<\/strong><\/em> exhibited the orange-to-red hues of ozone-rich air within the atmospheric column due to a lowered tropopause associated with the rapidly deepening North Atlantic storm.<\/p>\n<p><div style=\"width: 649px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/02\/190219_goes16_airmassRGB_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/02\/20190219213016_fulldisk.jpg\" alt=\"GOES-16 Air Mass RGB images [click to play animation | MP4]\" width=\"639\" height=\"639\" \/><\/a><p class=\"wp-caption-text\">GOES-16 Air Mass RGB images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/02\/190219_goes16_airmassRGB_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>Looking to the west with GOES-17, Full Disk animations of Visible and Water Vapor images are shown below.<\/p>\n<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\/2019\/02\/190219_goes17_visible_Full_Disk_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/02\/G17_FD_VIS_B2_19FEB2019_2019050_163034_GOES-17_0001PANEL.GIF\" alt=\"GOES-17 &quot;Red&quot; Visible (0.64 \u00b5m) images [click to play animation]\" width=\"640\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">GOES-17 &#8220;Red&#8221; Visible <em>(0.64 \u00b5m)<\/em> images [click to play animation]<\/p><\/div><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/02\/190219_goes17_waterVapor_Full_Disk_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/02\/G17_FD_WV_B9_19FEB2019_2019050_163034_GOES-17_0001PANEL.GIF\" alt=\"GOES-17 Mid-level Water Vapor (6.9 \u00b5m) images [click to play animation]\" width=\"640\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">GOES-17 Mid-level Water Vapor<em> (6.9 \u00b5m)<\/em> images [click to play animation]<\/p><\/div>The more frequent 10-minute images allowed a short-lived signature of orographic waves within a transient dry slot immediately downwind <em>(northeast)<\/em> of Atka (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/02\/190219_PAAK_SFCMG.GIF\"><strong>PAAK<\/strong><\/a>) in the Aleutian Islands of Alaska\u00a0 <em><strong>(below)<\/strong><\/em> &#8212; such a signature often indicates a high potential of turbulence. There were also areas of transverse banding seen with the <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/02\/190219_npac_mslp_250jet_anim.gif\"><strong>jet stream<\/strong><\/a> cirrus just southeast of Atka (another satellite signature of turbulence).<\/p>\n<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\/2019\/02\/190219_goes17_waterVapor_Aleutians_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/02\/G17_WV_ALEUTIANS_19FEB2019_2019050_213033_GOES-17_0002PANELS.GIF\" alt=\"GOES-17 Low-level (7.3 \u00b5m) and Mid-level (6.9 \u00b5m) Water Vapor images [click to play animation]\" width=\"640\" height=\"479\" \/><\/a><p class=\"wp-caption-text\">GOES-17 Low-level<em> (7.3 \u00b5m, left)<\/em> and Mid-level <em>(6.9 \u00b5m, right)<\/em> Water Vapor images [click to play animation]<\/p><\/div>Similar to what was seen over the North Atlantic, GOES-17 Air Mass RGB images <em><strong>(below)<\/strong><\/em> exhibited the orange-to-red hues of ozone-rich air within the atmospheric column due to a lowered tropopause poleward of the jet stream axis as it moved northeastward across the Aleutians.<\/p>\n<div style=\"width: 649px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/02\/190219_goes17_airmassRGB_Alaska_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/02\/20190219213033_ak.jpg\" alt=\"GOES-17 Air Mass RGB images [click to play animation | MP4]\" width=\"639\" height=\"242\" \/><\/a><p class=\"wp-caption-text\">GOES-17 Air Mass RGB images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/02\/190219_goes17_airmassRGB_Alaska_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>Both GOES-16 (GOES-East) and GOES-17 (GOES-West) were placed into the Mode 6 scan strategy for a 3-day period of testing beginning at 1500 UTC on 19\u00a0 February 2019 &#8212; which provides Full Disk images every 10 minutes (instead of every 15 minutes for the more common Mode 3 scan strategy). Further details on GOES-R series [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":31926,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[74,80,45],"tags":[],"class_list":["post-31922","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-16","category-goes-17","category-redgreenblue-rgb-images"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/31922","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=31922"}],"version-history":[{"count":15,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/31922\/revisions"}],"predecessor-version":[{"id":31941,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/31922\/revisions\/31941"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/31926"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=31922"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=31922"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=31922"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}