{"id":41721,"date":"2021-08-02T23:01:00","date_gmt":"2021-08-02T23:01:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=41721"},"modified":"2021-08-06T01:42:56","modified_gmt":"2021-08-06T01:42:56","slug":"sun-glint-and-calm-winds","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/41721","title":{"rendered":"Sun glint and calm winds"},"content":{"rendered":"\n<p>True-color imagery from the <a rel=\"noreferrer noopener\" href=\"https:\/\/ge.ssec.wisc.edu\/viirs-today\/\" target=\"_blank\">VIIRS Today website<\/a>, below (click <a href=\"https:\/\/ge.ssec.wisc.edu\/viirs-today\/index.php?satellite=n2&amp;product=true_color&amp;date=2021_08_02_214&amp;overlay_sector=false&amp;overlay_state=true&amp;overlay_coastline=true&amp;sector=USA7&amp;resolution=2000m\">here <\/a>for a direct link to the image below at the VIIRS Today site), shows an unusual sunglint pattern over the eastern Gulf of Mexico, to the southwest of the Florida peninsula.  Typically, sunglint features are fairly wide in VIIRS imagery, as evidenced from <a href=\"https:\/\/ge.ssec.wisc.edu\/viirs-today\/index.php?satellite=n1&amp;product=true_color&amp;date=2021_08_02_214&amp;overlay_sector=false&amp;overlay_state=true&amp;overlay_coastline=true&amp;sector=USA8&amp;resolution=2000m\">this Suomi-NPP image<\/a>, also from 2 August, but to the east of Florida.  However, the winds over the eastern Gulf were very light on 2 August, so surface wave action was reduced.  When the ocean approaches glassy calm, solar reflection becomes more unidirectional, and a brighter spot becomes visible in True-Color imagery.  When seas are choppier (as was the case to the east of Florida), solar reflection off the ocean is diffuse, and a less concentrated region of brightness results.  An good analogy might be reflection off flat aluminum foil (representing a flat sea state) or very crinkled aluminum foil (representing an agitated sea state). <\/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\/2021\/08\/noaa20_TrueColor_2August2021.21214.USA7_.143.2000m.jpg\"><img loading=\"lazy\" decoding=\"async\" width=\"650\" height=\"750\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/noaa20_TrueColor_2August2021.21214.USA7_.143.2000m.jpg\" alt=\"\" class=\"wp-image-41722\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/noaa20_TrueColor_2August2021.21214.USA7_.143.2000m.jpg 650w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/noaa20_TrueColor_2August2021.21214.USA7_.143.2000m-260x300.jpg 260w\" sizes=\"auto, (max-width: 650px) 100vw, 650px\" \/><\/a><figcaption>NOAA-20 True Color Imagery over the eastern Gulf of Mexico from 2 August 2021 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>What evidence is present of light winds?  Consider the Metop-A Scatterometry image, below, from <a href=\"https:\/\/www.ospo.noaa.gov\/Products\/atmosphere\/ascat\/winds.html\">this site<\/a>.  Both the <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/MetopAAscendingPass_2August2021.png\">ascending pass<\/a> (about 0145 UTC) and descending pass, below (about 1410 UTC;  orbit imagery available <a href=\"https:\/\/www.ssec.wisc.edu\/datacenter\/polar_orbit_tracks\/data\/METOP-A\/2021\/2021_08_02_214\/NA.gif\">here<\/a>, from <a href=\"https:\/\/www.ssec.wisc.edu\/datacenter\/polar_orbit_tracks\/\">this site<\/a>) show very weak winds over the Gulf to the southwest of Florida.<\/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\/2021\/08\/MetopADescendingPass.png\"><img loading=\"lazy\" decoding=\"async\" width=\"740\" height=\"650\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/MetopADescendingPass.png\" alt=\"\" class=\"wp-image-41723\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/MetopADescendingPass.png 740w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/MetopADescendingPass-300x264.png 300w\" sizes=\"auto, (max-width: 740px) 100vw, 740px\" \/><\/a><figcaption>Metop-A Scatterometer winds from the ca. 1410 UTC descending pass, 2 August 2021 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<hr class=\"wp-block-separator\" \/>\n\n\n\n<p>The effect of the sun glint occurs in both visible and shortwave infrared channels.  The imagery below, downloaded from the CIMSS Direct Broadcast ftp site (<a href=\"https:\/\/ftp.ssec.wisc.edu\/pub\/eosdb\/j01\/viirs\/\">https:\/\/ftp.ssec.wisc.edu\/pub\/eosdb\/j01\/viirs\/<\/a>, from this ephemeral site &#8212; <a href=\"https:\/\/ftp.ssec.wisc.edu\/pub\/eosdb\/j01\/viirs\/2021_08_02_214_1837\/images\/\">https:\/\/ftp.ssec.wisc.edu\/pub\/eosdb\/j01\/viirs\/2021_08_02_214_1837\/images\/<\/a> &#8212; in particular), shows the five Image bands from VIIRS, a prominent signal is apparent in all but the longest wavelength.<\/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\/2021\/08\/noaa20_viirs_i01_to_i05_20210802_183724_annotate.step_.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"604\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/noaa20_viirs_i01_to_i05_20210802_183724_annotate.step_-1024x604.gif\" alt=\"\" class=\"wp-image-41731\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/noaa20_viirs_i01_to_i05_20210802_183724_annotate.step_-1024x604.gif 1024w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/noaa20_viirs_i01_to_i05_20210802_183724_annotate.step_-300x177.gif 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/noaa20_viirs_i01_to_i05_20210802_183724_annotate.step_-768x453.gif 768w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a><figcaption>NOAA-20 VIIRS I-Bands 01-05 over the southeastern Gulf of Mexico, 1842 UTC on 2 August 2021 (Click to animate)<\/figcaption><\/figure>\n\n\n\n<p>Does the sunglint affect products?  The Cloud Mask product is tricked by the large reflectance into believing a cloud is present, as highlighted by the box below.  The image also includes Cloud Type and Cloud Phase.  Because liquid water clouds are believed present, the ACSPO Sea-surface temperature algorithm (at bottom) produces no values in that region.  Careful inspection of the image, however, shows marginally warmer waters (a lighter pink color is apparent) adjacent to the sunglint where the lack of wind means surface mixing of waters is suppressed and a thin layer of very warm water can develop on the top of the ocean.<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"576\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/CLAVRXCloudMask_Phase_Type_1842UTC_02August2021-1024x576.png\" alt=\"\" class=\"wp-image-41738\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/CLAVRXCloudMask_Phase_Type_1842UTC_02August2021-1024x576.png 1024w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/CLAVRXCloudMask_Phase_Type_1842UTC_02August2021-300x169.png 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/CLAVRXCloudMask_Phase_Type_1842UTC_02August2021-768x432.png 768w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/CLAVRXCloudMask_Phase_Type_1842UTC_02August2021.png 1280w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><figcaption>CLAVR-X Cloud Mask product, 1842 UTC on 2 August 2021, along with Cloud Type (upper right) and Cloud Phase (lower right).<\/figcaption><\/figure>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"604\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/n20_viirs_sst_20210802_183724_annotate-1024x604.png\" alt=\"\" class=\"wp-image-41735\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/n20_viirs_sst_20210802_183724_annotate-1024x604.png 1024w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/n20_viirs_sst_20210802_183724_annotate-300x177.png 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/n20_viirs_sst_20210802_183724_annotate-768x453.png 768w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/n20_viirs_sst_20210802_183724_annotate.png 1340w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><figcaption>ACSPO SSTs at 1842 UTC on 4 August 2021<\/figcaption><\/figure>\n\n\n\n<hr class=\"wp-block-separator\" \/>\n\n\n\n<p><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/noaa20_viirs_m01_to_m16_20210802_183724_annotate_step.gif\">This animation<\/a> steps through all the VIIRS M-bands.  The sunglint is apparent in nearly all of them, except for wavelengths longer than 4  \u00b5m.  The sunglint is also missing from the 1.38 \u00b5m (M09) imagery because of strong absorption of energy at that wavelength by water vapor.<\/p>\n\n\n\n<p>Other examples of diagnosing areas of light winds over water (via a lack of sunglint or moonglint) can be found <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/2669\">here<\/a>, <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/5488\">here<\/a>, <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/12735\">here<\/a> and <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/14212\">here<\/a>.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>True-color imagery from the VIIRS Today website, below (click here for a direct link to the image below at the VIIRS Today site), shows an unusual sunglint pattern over the eastern Gulf of Mexico, to the southwest of the Florida peninsula. Typically, sunglint features are fairly wide in VIIRS imagery, as evidenced from this Suomi-NPP [&hellip;]<\/p>\n","protected":false},"author":19,"featured_media":41731,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[58,78,25,48],"tags":[],"class_list":["post-41721","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-metop","category-noaa-20","category-satellite-winds","category-viirs"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/41721","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=41721"}],"version-history":[{"count":17,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/41721\/revisions"}],"predecessor-version":[{"id":41781,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/41721\/revisions\/41781"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/41731"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=41721"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=41721"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=41721"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}