{"id":65621,"date":"2025-06-30T16:13:21","date_gmt":"2025-06-30T16:13:21","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=65621"},"modified":"2025-07-04T16:54:38","modified_gmt":"2025-07-04T16:54:38","slug":"smog-with-light-winds-over-kyushu","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/65621","title":{"rendered":"Smog with light winds over Kyushu"},"content":{"rendered":"\n<figure class=\"wp-block-image size-large is-resized\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2025\/06\/N21_SNPP_N20_TrueColor_30June2025step.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"1605\" height=\"1181\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2025\/06\/N21_SNPP_N20_TrueColor_30June2025step.gif\" alt=\"\" class=\"wp-image-65625\"\/><\/a><figcaption class=\"wp-element-caption\">True Color imagery from NOAA-21 (ca. 0422 UTC), Suomi-NPP (ca. 0448 UTC) and NOAA-20 (ca. 0510 UTC) , 30 June 2025 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>True Color imagery over western Japan, above, from three JPSS Satellites (<a href=\"https:\/\/worldview.earthdata.nasa.gov\/?v=123.06170467059573,28.28220829718866,140.6806312904001,37.24678662590516&amp;l=Reference_Labels_15m(hidden),Reference_Features_15m(hidden),Coastlines_15m,VIIRS_NOAA20_AOT_Dark_Target_Land_Ocean(hidden),VIIRS_SNPP_AOT_Dark_Target_Land_Ocean(hidden),VIIRS_SNPP_Thermal_Anomalies_375m_Day,VIIRS_NOAA21_Thermal_Anomalies_375m_Day(hidden),VIIRS_NOAA20_Thermal_Anomalies_375m_Day,VIIRS_NOAA21_CorrectedReflectance_TrueColor(hidden),VIIRS_NOAA20_CorrectedReflectance_TrueColor,VIIRS_SNPP_CorrectedReflectance_TrueColor(hidden),MODIS_Aqua_CorrectedReflectance_TrueColor(hidden),MODIS_Terra_CorrectedReflectance_TrueColor(hidden)&amp;lg=true&amp;t=2025-06-30-T12%3A40%3A38Z\">from the NASA Worldview site<\/a>) show a region with a hazy signature that appears to originate over Kyushu&#8217;s main cities of Kumamoto and Fukuoka. Winds at this time are relatively light, as evidenced by the NOAA-21 image, shown below, that includes a dark region within the sun glint (see <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/41721\">this blog post<\/a> for another discussion of diagnosing light winds within areas of sun glint).<\/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\/2025\/06\/NOAA-21_TrueColor_30June2025rT_circledtoggle.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"1605\" height=\"1181\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2025\/06\/NOAA-21_TrueColor_30June2025rT_circledtoggle.gif\" alt=\"\" class=\"wp-image-65626\"\/><\/a><figcaption class=\"wp-element-caption\">NOAA-21 True Color imagery ca. 0422 UTC on 30 June 2025 (Click to enlarge).  A region of likely light winds is circled.<\/figcaption><\/figure>\n\n\n\n<p>Advanced Scattermeter (ASCAT) data from a fortuitous overpass from Metop-B (<a href=\"https:\/\/manati.star.nesdis.noaa.gov\/datasets\/ASCATBData.php\">source<\/a>), shown below, confirms the region of very light winds around Kyushu.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full is-resized\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2025\/06\/MetopB_ASCATWinds_1229UTC_30June2025.png\"><img loading=\"lazy\" decoding=\"async\" width=\"740\" height=\"650\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2025\/06\/MetopB_ASCATWinds_1229UTC_30June2025.png\" alt=\"\" class=\"wp-image-65630\" style=\"width:1086px;height:auto\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2025\/06\/MetopB_ASCATWinds_1229UTC_30June2025.png 740w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2025\/06\/MetopB_ASCATWinds_1229UTC_30June2025-300x264.png 300w\" sizes=\"auto, (max-width: 740px) 100vw, 740px\" \/><\/a><figcaption class=\"wp-element-caption\">ASCAT winds from MetopB, 1229 UTC on 30 June 2025 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>Aerosol Optical Depth (scaled from 0-5) computed from Suomi NPP and NOAA-20 is shown below.  The haze does not appear to be from active fires based on <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2025\/06\/H9Band07-20250630_0300_to_0600_by10anim.gif\">this animation of shortwave infrared imagery from Himawari-9<\/a>.<\/p>\n\n\n\n<figure class=\"wp-block-image size-large is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"1605\" height=\"1181\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2025\/06\/SNPP_N20_AOD_30June2025rT.png\" alt=\"\" class=\"wp-image-65627\" style=\"width:1086px;height:auto\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2025\/06\/SNPP_N20_AOD_30June2025rT.png 1605w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2025\/06\/SNPP_N20_AOD_30June2025rT-300x221.png 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2025\/06\/SNPP_N20_AOD_30June2025rT-1024x753.png 1024w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2025\/06\/SNPP_N20_AOD_30June2025rT-768x565.png 768w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2025\/06\/SNPP_N20_AOD_30June2025rT-1536x1130.png 1536w\" sizes=\"auto, (max-width: 1605px) 100vw, 1605px\" \/><figcaption class=\"wp-element-caption\">Aerosol Optical Depth imagery (blended from Suomi-NPP and NOAA-20), 30 June 2025 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>Air Quality Indices, below, (<a href=\"https:\/\/www.iqair.com\/us\/japan\/fukuoka?srsltid=AfmBOoqh5a_d-pUYRb4OUvE4Z-7ucX5UJyYRabxFcX-MLbXyAiLTZI0G\">from this site<\/a>), show the worst near-surface Air Quality over southern Kyushu.  This is a good reminder that satellite detection of AOD views the entire atmosphere &#8212; to get the best description of Air Quality, use both surface and satellite detection.<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"386\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2025\/06\/AQI_Japan_30June2025-1024x386.png\" alt=\"\" class=\"wp-image-65628\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2025\/06\/AQI_Japan_30June2025-1024x386.png 1024w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2025\/06\/AQI_Japan_30June2025-300x113.png 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2025\/06\/AQI_Japan_30June2025-768x290.png 768w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2025\/06\/AQI_Japan_30June2025.png 1227w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><figcaption class=\"wp-element-caption\">Near-surface Air Quality over southwestern Japan, 30 June 2025 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<p>Editor&#8217;s Note: This is my last contribution to the CIMSS Satellite Blog, as I am retiring today after 30 years (plus 1 month, a week and a day) with the University of Wisconsin-Madison. It has been a great honor to talk about beautiful and informative satellite imagery in this space, starting in 2006 <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/217\">with this blog post on Parallax<\/a>. I hope my writings (1) have been helpful and (2) have been accurate.  It&#8217;s honestly the best job I could imagine having!<\/p>\n","protected":false},"excerpt":{"rendered":"<p>True Color imagery over western Japan, above, from three JPSS Satellites (from the NASA Worldview site) show a region with a hazy signature that appears to originate over Kyushu&#8217;s main cities of Kumamoto and Fukuoka. Winds at this time are relatively light, as evidenced by the NOAA-21 image, shown below, that includes a dark region [&hellip;]<\/p>\n","protected":false},"author":19,"featured_media":65622,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[7,73,78,131,49],"tags":[],"class_list":["post-65621","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-air-quality","category-himawari-9","category-noaa-20","category-noaa-21","category-suomi_npp"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/65621","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=65621"}],"version-history":[{"count":6,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/65621\/revisions"}],"predecessor-version":[{"id":65738,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/65621\/revisions\/65738"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/65622"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=65621"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=65621"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=65621"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}