{"id":37241,"date":"2020-06-15T20:48:25","date_gmt":"2020-06-15T20:48:25","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=37241"},"modified":"2020-06-18T12:23:42","modified_gmt":"2020-06-18T12:23:42","slug":"detection-of-saharan-air-layer-in-the-eastern-atlantic","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/37241","title":{"rendered":"Detection of Saharan Air Layer in the eastern Atlantic"},"content":{"rendered":"
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Color-enhanced GOES-16 Split Window Difference field, 1500 UTC on 15 June 2020 (Click to enlarge)<\/p><\/div>\n

GOES-16 Split Window difference (SWD) fields, above, and Meteosat Dust RGB<\/a> imagery (both from 1500 UTC on 15 June 2020, and available at this site<\/a>) suggest that a Saharan Air Layer (SAL) event is developing in the eastern Atlantic Ocean.\u00a0 (Click here <\/a>to see an animation of the Split Window Difference; AWIPS note: the default SWD enhancement has been replaced in the animation by the Grid\/Low-Range Enhanced field) The dry, dusty air associated with SALs has an impact on air quality in the Caribbean, and it also suppresses tropical cyclone activity.\u00a0 What other satellite products can be used to track this feature?<\/p>\n

The 4-panel images below includes GOES-16 Aerosol Detection (upper left), GOES-16 Dust RGB (upper right), GOES-16 Split-Window Difference (10.3 \u00b5m – 12.3 \u00b5m) (lower left), and gridded NOAA-Unique Combined Atmospheric Processing System (NUCAPS) 850-700 mb Relative Humidity at 1550 UTC`and 1600 UTC. GOES-16 Aerosol Detection can detect SAL layers because of the suspended dust in the atmosphere. Both the Dust RGB and Split Window difference fields detect the SAL because of the differential absorption of infrared radiation at 10.3 \u00b5m and 12.3 \u00b5m by silicates within the dust.\u00a0 <\/p>\n

The bright pink in the Dust RGB is characteristic of dust detection with that product, and it shows a strong feature emerging from Africa.\u00a0 The Split Window difference (SWD) field shows the SAL region to be blue to brown;\u00a0 note that SAL air is indicated over the central Atlantic as well.\u00a0 The yellow\/orange\/red enhancement in the SWD (bracketed by blue regions in the enhancement that suggest dry air) between 30\u00ba and 40\u00ba W Longitude, and 10\u00ba and 20\u00ba N Latitude, suggests more moisture in the air there.<\/p>\n

Aerosol Optical Depth is higher in the SAL air because of the suspended dust.\u00a0 Relatively cleaner air is north and south of the feature.\u00a0 The low-level Relative Humidity in the SAL air is low.\u00a0 This is more easily seen in the later image — 1600 UTC with this ascending NOAA-20 pass — than in the earlier (1550 UTC) image.\u00a0 (Click here<\/a> to see a toggle of both gridded NUCAPS fields).<\/p>\n

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GOES-16 Aerosol Detection (upper left), GOES-16 Dust RGB (upper right), GOES-16 Split-Window Difference (10.3 \u00b5m – 12.3 \u00b5m) (lower left), and gridded NOAA-Unique Combined Atmospheric Processing System (NUCAPS) 850-700 mb Relative Humidity at 1550 UTC (Click to enlarge)<\/p><\/div>\n

\"\"<\/a>

GOES-16 Aerosol Detection (upper left), GOES-16 Dust RGB (upper right), GOES-16 Split-Window Difference (10.3 \u00b5m – 12.3 \u00b5m) (lower left), and gridded NOAA-Unique Combined Atmospheric Processing System (NUCAPS) 850-700 mb Relative Humidity at 1600 UTC (Click to enlarge)<\/p><\/div>\n

GOES-16 Aerosol Products, below, identify both the region of higher Aerosol Optical Depth (AOD), and the type of Aerosol (in this case:\u00a0 Dust) that is responsible for the higher AOD values.<\/p>\n

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GOES-16 Aerosol Optical Depth and GOES-16 Aerosol Type, 1600 UTC on 15 June 2020 (Click to enlarge)<\/p><\/div>\n

The plot below shows the location of the NUCAPS points for the early afternoon swath in the eastern Atlantic. The points overlay the 850 mb – 700 mb relative humidity fields. Note the dryness at the eastern edge of the image, near 30\u00ba W; a skinny tongue of moisture (cyan in the moisture enhancement) extends to the north (corresponding to the region in the SWD where yellow\/orange\/red colors suggest more moisture), with dry air north and west of that moisture, near 45\u00ba W. <\/p>\n

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NUCAPS Sounding Locations overlain on top of Gridded NUCAPS field of 850 mb – 700 mb relative humidity (Click to enlarge)<\/p><\/div>\n

The three soundings below show the dry air to the north and west (13\u00ba N, 42.5\u00ba W), the relative moisture in the middle (13.5\u00ba N, 36.5\u00ba W), and the dry air to the east (13.5\u00ba N, 31\u00ba W).<\/p>\n

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NUCAPS soundings at 1600 UTC in dry air, in the ribbon of moist air, and in dry air at the eastern edge of the NUCAPS swath.<\/p><\/div>\n

True-color imagery (an example computed using CSPP-Geo is shown below from 1710 UTC) can also be used to track dust.\u00a0 Dust in true color has a much different presentation than adjacent clear(er) skies.<\/p>\n

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GOES-16 True Color imagery, 1730 UTC on 15 June 2020 (Click to enlarge)<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"

GOES-16 Split Window difference (SWD) fields, above, and Meteosat Dust RGB imagery (both from 1500 UTC on 15 June 2020, and available at this site) suggest that a Saharan Air Layer (SAL) event is developing in the eastern Atlantic Ocean.\u00a0 (Click here to see an animation of the Split Window Difference; AWIPS note: the default […]<\/p>\n","protected":false},"author":19,"featured_media":37248,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[7,74,78,83],"tags":[],"class_list":["post-37241","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-air-quality","category-goes-16","category-noaa-20","category-nucaps"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/37241","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=37241"}],"version-history":[{"count":10,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/37241\/revisions"}],"predecessor-version":[{"id":37261,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/37241\/revisions\/37261"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/37248"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=37241"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=37241"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=37241"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}