{"id":10039,"date":"2012-03-22T20:58:23","date_gmt":"2012-03-22T20:58:23","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=10039"},"modified":"2012-03-26T17:29:27","modified_gmt":"2012-03-26T17:29:27","slug":"using-polar-orbiter-modis-imagery-to-supplement-degraded-geostationary-goes-imagery","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/10039","title":{"rendered":"Using polar-orbiter MODIS and AVHRR imagery to supplement degraded geostationary GOES imagery"},"content":{"rendered":"<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/03\/120321_modis_goes13_wv_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"MODIS 6.7 \u00c2\u00b5m water vapor image + GOES-13 6.5 \u00c2\u00b5m water vapor image\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/03\/120321_modis_goes13_wv_anim.gif\" alt=\"MODIS 6.7 \u00c2\u00b5m water vapor image + GOES-13 6.5 \u00c2\u00b5m water vapor image\" width=\"480\" height=\"396\" \/><\/a><p class=\"wp-caption-text\">MODIS 6.7 \u00c2\u00b5m water vapor image + GOES-13 6.5 \u00c2\u00b5m water vapor image\u00c2 <\/p><\/div>\n<p>After 20:30 UTC on <a title=\"21 March 2012 daily weather map\" href=\"http:\/\/www.hpc.ncep.noaa.gov\/dailywxmap\/index_20120321.html\"><strong>21 March 2012<\/strong><\/a>, GOES-15 <em>(GOES West)<\/em> experienced a bad momentum unload, and at this point the satellite went into\u00c2\u00a0 a sun acquisition mode (a &#8220;safe mode&#8221;) and stopped transmitting data (<a title=\"latest GOES-15 status messages\" href=\"http:\/\/www.ssd.noaa.gov\/PS\/SATS\/MESS\/MSG0831638.02.txt\"><strong>latest GOES-15 status messages<\/strong><\/a>). NOAA\/NESDIS immediately began to operate GOES-13 <em>(GOES East)<\/em> in continuous Full Disk scan mode, in order to provide imagery as far west as possible every 30 minutes. However, due to the extreme viewing angle from GOES-13 <em>(positioned over the Equator at 75 degrees West longitude),<\/em> the image quality over the western US was degraded (since the effective pixel resolution was so large). In addition, Alaska, Hawaii, and the Pacific Region were effectively <a title=\"GOES-West \/ GOES-East IR image composite animation\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/03\/120321-22_goes_pacific_region_anim.gif\"><strong>without useful GOES imagery<\/strong><\/a> (although some of these areas could make use of Japanese <a title=\"MTSAT imagery\" href=\"http:\/\/www.ssec.wisc.edu\/data\/geo\/index.php?satellite=mtsat&amp;channel=ir2&amp;coverage=fd&amp;file=gif&amp;imgoranim=8&amp;anim_method=flash\"><strong>MTSAT imagery<\/strong><\/a> to help fill the GOES-15 imagery gap).<\/p>\n<p>Shortly after the GOES-15 outage, AWIPS comparisons of a 1-km resolution MODIS 6.7 \u00c2\u00b5m water vapor image with the corresponding GOES-13 6.5 \u00c2\u00b5m water vapor image <em><strong>(above)<\/strong><\/em> as well as the MODIS 11.0 \u00c2\u00b5m IR channel image and the corresponding GOES-13 10.7 \u00c2\u00b5m IR image <em><strong>(below)<\/strong><\/em> demonstrate the value of using higher spatial resolution polar-orbiter <em>(from the Terra and Aqua satellites)<\/em> MODIS imagery to supplement the degraded geostationary GOES-13 imagery during the GOES-15 outage. In these 2 examples, the GOES-13 viewing angle for San Francisco, California is 65 degrees, making the effective resolution of the &#8220;4 km&#8221; IR and water vapor image pixels closer to 16 km. In addition, the large satellite viewing angles were creating a significant &#8220;<a title=\"parallax error\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/217\"><strong>parallax error<\/strong><\/a>&#8220;, shifting the apparent location of high cloud features to the northwest.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/03\/120321_modis_goes13_ir_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"MODIS 11.0 \u00c2\u00b5m IR image + GOES-13 10.7 \u00c2\u00b5m IR image\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/03\/120321_modis_goes13_ir_anim.gif\" alt=\"MODIS 11.0 \u00c2\u00b5m IR image + GOES-13 10.7 \u00c2\u00b5m IR image\" width=\"480\" height=\"396\" \/><\/a><p class=\"wp-caption-text\">MODIS 11.0 \u00c2\u00b5m IR image + GOES-13 10.7 \u00c2\u00b5m IR image<\/p><\/div>\n<p style=\"text-align: center;\">========================================================<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/03\/120322_modis_goes13_wv_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"MODIS 6.7 \u00c2\u00b5m water vapor image + GOES-13 6.5 \u00c2\u00b5m water vapor image\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/03\/120322_modis_goes13_wv_anim.gif\" alt=\"MODIS 6.7 \u00c2\u00b5m water vapor image + GOES-13 6.5 \u00c2\u00b5m water vapor image\" width=\"480\" height=\"395\" \/><\/a><p class=\"wp-caption-text\">MODIS 6.7 \u00c2\u00b5m water vapor image + GOES-13 6.5 \u00c2\u00b5m water vapor image<\/p><\/div>\n<p>On the following day,\u00c2\u00a0 AWIPS comparisons of a MODIS 6.7 \u00c2\u00b5m water vapor image with the corresponding GOES-13 6.5 \u00c2\u00b5m water vapor channel image <em><strong>(above)<\/strong><\/em> as well as a MODIS 11.0 \u00c2\u00b5m IR channel image with the corresponding GOES-13 10.7 \u00c2\u00b5m IR channel image <em><strong>(below)<\/strong><\/em> showed a storm moving into the far southern panhandle of Alaska. In the case, the GOES-13 satellite viewing angles for Seattle, Washington and Juneau, Alaska were 71 degrees and 82 degrees, respectively.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/03\/120322_modis_goes13_ir_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"MODIS 11.0 \u00c2\u00b5m IR image + GOES-13 10.7 \u00c2\u00b5m IR image\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/03\/120322_modis_goes13_ir_anim.gif\" alt=\"MODIS 11.0 \u00c2\u00b5m IR image + GOES-13 10.7 \u00c2\u00b5m IR image\" width=\"480\" height=\"396\" \/><\/a><p class=\"wp-caption-text\">MODIS 11.0 \u00c2\u00b5m IR image + GOES-13 10.7 \u00c2\u00b5m IR image<\/p><\/div>\n<p>Similarly, an AWIPS comparison of a 1-km resolution POES AVHRR 12.0 \u00c2\u00b5m IR image with the corresponding GOES-13 10.7 \u00c2\u00b5m IR image <em><strong>(below)<\/strong><\/em> shows another source for polar-orbiter satellite imagery to supplement GOES in this type of situation.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/03\/120322_avhrr_goes13_ir_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"POES AVHRR 12.0 \u00c2\u00b5m IR image + GOES-13 10.7 \u00c2\u00b5m IR image\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/03\/120322_avhrr_goes13_ir_anim.gif\" alt=\"POES AVHRR 12.0 \u00c2\u00b5m IR image + GOES-13 10.7 \u00c2\u00b5m IR image\" width=\"480\" height=\"396\" \/><\/a><p class=\"wp-caption-text\">POES AVHRR 12.0 \u00c2\u00b5m IR image + GOES-13 10.7 \u00c2\u00b5m IR image<\/p><\/div>\n<p>CIMSS participation in <a title=\"GOES-R Proving Ground\" href=\"..\/..\/goes_r\/proving-ground.html\"><strong>GOES-R Proving Ground<\/strong><\/a> activities includes making a variety of <a title=\"AVHRR imagery in AWIPS\" href=\"http:\/\/www.ssec.wisc.edu\/~jordang\/awips-avhrr\/index.html\"><strong>POES AVHRR<\/strong><\/a> and\u00c2\u00a0 <strong><a href=\"http:\/\/www.ssec.wisc.edu\/%7Ejordang\/awips-modis\/index.html\">MODIS<\/a><\/strong> images and products available for National Weather Service forecast offices to add to their local AWIPS workstations. Currently there are <strong><a title=\"NWS offices\" href=\"http:\/\/cimss.ssec.wisc.edu\/goes_r\/proving-ground\/awips\/awips-modis\/cwas.png\">57 NWS offices<\/a><\/strong> receiving MODIS imagery and products from CIMSS.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>After 20:30 UTC on 21 March 2012, GOES-15 (GOES West) experienced a bad momentum unload, and at this point the satellite went into\u00c2\u00a0 a sun acquisition mode (a &#8220;safe mode&#8221;) and stopped transmitting data (latest GOES-15 status messages). NOAA\/NESDIS immediately began to operate GOES-13 (GOES East) in continuous Full Disk scan mode, in order to [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[22,10,11,34,12,20,26],"tags":[],"class_list":["post-10039","post","type-post","status-publish","format-standard","hentry","category-avhrr","category-general-interpretation","category-goes-13","category-goes-r","category-modis","category-mtsat","category-poes"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/10039","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=10039"}],"version-history":[{"count":27,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/10039\/revisions"}],"predecessor-version":[{"id":10042,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/10039\/revisions\/10042"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=10039"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=10039"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=10039"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}