{"id":60404,"date":"2024-07-22T15:52:19","date_gmt":"2024-07-22T15:52:19","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=60404"},"modified":"2024-07-23T13:49:33","modified_gmt":"2024-07-23T13:49:33","slug":"viirs-estimates-of-smoke-over-the-central-united-states","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/60404","title":{"rendered":"VIIRS [added:  and GOES!] estimates of smoke over the central United States"},"content":{"rendered":"\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1524\" height=\"1008\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/VIIRSTrueColor_DNB_AOD-20240721_1925toggle.gif\" alt=\"\" class=\"wp-image-60405\"\/><figcaption class=\"wp-element-caption\">NOAA-20 True Color imagery, Day Night band visible (0.7 \u00b5m) imagery, and Aerosol Optical Depth (AOD) on 1925 UTC, 21 July 2024 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>As noted <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/60362\">here<\/a>, <a href=\"https:\/\/cimss.ssec.wisc.edu\/cspp\/\">CSPP software<\/a> now includes the ability to show reprojected values of Aerosol Optical Depth, in this case within AWIPS. The <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/VIIRSAOD-20240721_192548.png\">AOD from the NOAA-20 afternoon pass on 21 July<\/a> shows extensive smoke over the Plains of Canada and the northern Plains of the USA. Clean air is confined to the Upper Peninsula (UP) of Michigan. <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/VIIRSDNB-20240721_192548.png\">The Day Night band imagery at the same time<\/a> is more distinct over the UP as well.  Note, for example, how easy it is to see Lake Superior compared to Lake of the Woods on the Minnesota\/Canada border, or Lake Manitoba.<\/p>\n\n\n\n<p>AOD computation with VIIRS data requires <a href=\"https:\/\/rammb.cira.colostate.edu\/projects\/npp\/viirs_bands_and_bandwidths.pdf\">visible bands that give no information at night<\/a> (the ATBD for VIIRS AOD is <a href=\"https:\/\/www.star.nesdis.noaa.gov\/jpss\/documents\/ATBD\/ATBD_EPS_Aerosol_AOD_v3.4.pdf\">here<\/a>).  Day Night Band imagery &#8212; <a href=\"https:\/\/www.moongiant.com\/phase\/7\/22\/2024\">with a near-full moon<\/a> &#8212; gives information on smoke distribution based on, as above, how well surface features can be viewed.<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/VIIRSDNB-20240722_0745_0902toggle.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"1524\" height=\"1008\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/VIIRSDNB-20240722_0745_0902toggle.gif\" alt=\"\" class=\"wp-image-60411\"\/><\/a><figcaption class=\"wp-element-caption\">NOAA-20 VIIRS Day Night Band visible (0.7 \u00b5m) imagery, 0745 and 0902 UTC on 22 July 2024 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>VIIRS data from the CIMSS Direct Broadcast site &#8212; the source of these AWIPS images &#8212; can also be viewed online <a href=\"https:\/\/cimss.ssec.wisc.edu\/viirs\/imagery-viewer\/\">here<\/a>.<\/p>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<p>VIIRS AOD from the afternoon overpass on 22 July 2024, below, shows a general increase in AOD values over the midwest as the region of relatively clean air over the western Great Lakes shrinks.<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/VIIRSAOD-20240722_190553.png\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"677\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/VIIRSAOD-20240722_190553-1024x677.png\" alt=\"\" class=\"wp-image-60423\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/VIIRSAOD-20240722_190553-1024x677.png 1024w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/VIIRSAOD-20240722_190553-300x198.png 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/VIIRSAOD-20240722_190553-768x508.png 768w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/VIIRSAOD-20240722_190553.png 1524w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a><figcaption class=\"wp-element-caption\">VIIRS AOD from NOAA-20, 1905 UTC on 22 July 2024 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>Earth-based observations at Madison <a href=\"https:\/\/hsrl.ssec.wisc.edu\/by_site\/6\/2024\/07\/22\/am\">from this site<\/a> show the evolution of the particulate matter from 17-22 July.  There is an increase an lowering in the particulates over the course of time.  In particular, a defined layer near 4 km becomes apparent by 19 July 2024.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/ratioIR_20240717-22_15_stepanim.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"908\" height=\"935\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/ratioIR_20240717-22_15_stepanim.gif\" alt=\"\" class=\"wp-image-60424\"\/><\/a><figcaption class=\"wp-element-caption\">Aerosol backscatter at Madison WI, 17-22 July 2024 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>The smoke layer is also apparent in the series of small plots shown below, starting high in the atmosphere on 18 July, and descending to around 4 km on 19 July.  A lower-layer of particulates was also present on 19-21 July 2024;  showers on the 21st likely removed that lower layer.<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/SeriesOfSmallPlots.png\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"406\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/SeriesOfSmallPlots-1024x406.png\" alt=\"\" class=\"wp-image-60425\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/SeriesOfSmallPlots-1024x406.png 1024w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/SeriesOfSmallPlots-300x119.png 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/SeriesOfSmallPlots-768x304.png 768w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/SeriesOfSmallPlots.png 1110w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a><figcaption class=\"wp-element-caption\">Aerosol Backscatter, 13-22 July 2024 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<p>GOES-R Satellites also produce the Level 2 product Aerosol Optical Depth.  The animation below shows GOES-derived values from 1756-2201 UTC on 22 July.  The data are produced every 5 minutes, and the extensive smoke pall is captured.<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1524\" height=\"1008\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/G16AOD-20240722_1756_to_2201anim.gif\" alt=\"\" class=\"wp-image-60427\"\/><figcaption class=\"wp-element-caption\">GOES-16 Aerosol Optical Depth, 1756 &#8211; 2201 UTC on 22 July 2024 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>Four VIIRS overpasses occurred during the 5 hour animation shown above. The four toggles below compare the VIIRS and GOES-R AOD.  The VIIRS product on this day shows more coverage.  This is likely related to the different cloud masks.<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/GOES16_VIIRSAOD-20240722_1841toggle.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"1524\" height=\"1008\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/GOES16_VIIRSAOD-20240722_1841toggle.gif\" alt=\"\" class=\"wp-image-60429\"\/><\/a><figcaption class=\"wp-element-caption\">Aerosol Optical Depth estimates ca. 1841 UTC on 22 July 2024 from VIIRS and from GOES-16 ABI (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/GOES16_VIIRSAOD-20240722_1906toggle.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"1524\" height=\"1008\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/GOES16_VIIRSAOD-20240722_1906toggle.gif\" alt=\"\" class=\"wp-image-60430\"\/><\/a><figcaption class=\"wp-element-caption\">Aerosol Optical Depth estimates ca. 1906 UTC on 22 July 2024 from VIIRS and from GOES-16 ABI (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/GOES16_VIIRSAOD-20240722_2031toggle.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"1524\" height=\"1008\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/GOES16_VIIRSAOD-20240722_2031toggle.gif\" alt=\"\" class=\"wp-image-60431\"\/><\/a><figcaption class=\"wp-element-caption\">Aerosol Optical Depth estimates ca. 2031 UTC on 22 July 2024 from VIIRS and from GOES-16 ABI (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<figure class=\"wp-block-image size-large is-resized\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/GOES16_VIIRSAOD-20240722_2051toggle.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"1524\" height=\"1008\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/07\/GOES16_VIIRSAOD-20240722_2051toggle.gif\" alt=\"\" class=\"wp-image-60432\" style=\"width:1077px;height:auto\"\/><\/a><figcaption class=\"wp-element-caption\">Aerosol Optical Depth estimates ca. 2056 UTC on 22 July 2024 from VIIRS and from GOES-16 ABI (Click to enlarge)<\/figcaption><\/figure>\n","protected":false},"excerpt":{"rendered":"<p>As noted here, CSPP software now includes the ability to show reprojected values of Aerosol Optical Depth, in this case within AWIPS. The AOD from the NOAA-20 afternoon pass on 21 July shows extensive smoke over the Plains of Canada and the northern Plains of the USA. Clean air is confined to the Upper Peninsula [&hellip;]<\/p>\n","protected":false},"author":19,"featured_media":60406,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[7,78,48],"tags":[],"class_list":["post-60404","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-air-quality","category-noaa-20","category-viirs"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/60404","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=60404"}],"version-history":[{"count":8,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/60404\/revisions"}],"predecessor-version":[{"id":60434,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/60404\/revisions\/60434"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/60406"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=60404"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=60404"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=60404"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}