{"id":31455,"date":"2019-01-23T23:59:57","date_gmt":"2019-01-23T23:59:57","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=31455"},"modified":"2019-01-24T15:29:50","modified_gmt":"2019-01-24T15:29:50","slug":"dry-air-aloft-over-the-western-atlantic-ocean","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/31455","title":{"rendered":"Dry air aloft over the western Atlantic Ocean"},"content":{"rendered":"<p><div style=\"width: 653px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/01\/190123_goes16_waterVapor_Atlantic_marine_stratocumulus_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/01\/atl_wv-20190123_180216.png\" alt=\"GOES-16 Mid-level Water Vapor (6.9 \u00b5m) images, with plots of rawinsonde sites in yellow [click to play animation | MP4]\" width=\"643\" height=\"371\" \/><\/a><p class=\"wp-caption-text\">GOES-16 Mid-level Water Vapor <em>(6.9 \u00b5m)<\/em> images, with rawinsonde sites plotted in yellow [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/01\/190123_goes16_waterVapor_Atlantic_marine_stratocumulus_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>With a <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/01\/atl_wv_500height-20190123_180216.png\"><strong>ridge of high pressure<\/strong><\/a> in place over the western Atlantic Ocean, GOES-16 <em>(GOES-East)<\/em> Mid-level Water Vapor (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band09.pdf\"><strong>6.9 \u00b5m<\/strong><\/a>) images <em><strong>(above)<\/strong><\/em> indicated the presence of dry air within the middle troposphere off the Southeast US coast on 23 January 2019.<\/p>\n<p>GOES-16 &#8220;Red&#8221; Visible (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band02.pdf\"><strong>0.64 \u00b5m<\/strong><\/a>) images showed that marine boundary layer stratocumulus clouds covered much of this region of the Atlantic &#8212; and due to minimal absorption by mid-tropospheric water vapor, these stratocumulus clouds were also very apparent in the corresponding GOES-16 Near-Infrared &#8220;Cirrus&#8221; (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band04.pdf\"><strong>1.38 \u00b5m<\/strong><\/a>) images <em><strong>(below)<\/strong><\/em>.<\/p>\n<p><div style=\"width: 649px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/01\/190123_goes16_visible_cirrus_Atlantic_marine_stratocumulus_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/01\/atl_cirrus-20190123_180216.png\" alt=\"GOES-16 &quot;Red&quot; Visible (0.64 \u00b5m) and Near-Infrared &quot;Cirrus&quot; (1.37 \u00b5m) images, with plots of rawinsonde sites in yellow [click to play animation | MP4]\" width=\"639\" height=\"369\" \/><\/a><p class=\"wp-caption-text\">GOES-16 &#8220;Red&#8221; Visible<em> (0.64 \u00b5m)<\/em> and Near-Infrared &#8220;Cirrus&#8221;<em> (1.38 \u00b5m)<\/em> images, with rawinsonde sites plotted in yellow [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/01\/190123_goes16_visible_cirrus_Atlantic_marine_stratocumulus_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>Terra MODIS Visible (0.65 \u00b5m) and Near-Infrared &#8220;Cirrus&#8221; (1.38 \u00b5m) images at 1513 UTC <strong><em>(below)<\/em><\/strong> also showed a clear signature of the stratocumulus clouds at 1.38 \u00b5m.<\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/01\/190123_1513utc_terra_modis_visible_cirrus_Atlantic_marine_stratocumulus_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/01\/190123_1513utc_terra_modis_visible_cirrus_Atlantic_marine_stratocumulus_anim.gif\" alt=\"Terra MODIS Visible &lt;em&gt;(0.65 \u00b5m)&lt;\/em&gt; and Near-Infrared &quot;Cirrus&quot; &lt;em&gt;(1.38 \u00b5m)&lt;\/em&gt; images at 1513 UTC, with plots of rawinsonde sites in yellow [click to enlarge]\" width=\"641\" height=\"370\" \/><\/a><p class=\"wp-caption-text\">Terra MODIS Visible <em>(0.65 \u00b5m)<\/em> and Near-Infrared &#8220;Cirrus&#8221; <em>(1.38 \u00b5m)<\/em> images at 1513 UTC, with rawinsonde sites plotted in yellow [click to enlarge]<\/p><\/div>Cross sections of GFS90 model fields along <strong>Line I-I&#8217;<\/strong> &#8212; oriented from <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/01\/190123_12UTC_KCHS_RAOB.GIF\"><strong>Charleston, South Carolina<\/strong><\/a> to <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/01\/190123_12UTC_TXKF_RAOB.GIF\"><strong>Bermuda<\/strong><\/a> &#8212; are shown below. Note the very dry air within the middle troposphere, with Specific Humidity values of less than 0.2 g\/kg and Relative Humidity values less than 10% centered around the 500 hPa pressure level. In addition, the depth of the moist marine boundary layer was higher to the west at Charleston <em>(2.6 km, at 746 hPa)<\/em> than to the east at Bermuda <em>(1.9 km, at 822 hPa)<\/em>.<\/p>\n<div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/01\/190123_18utc_gfs90_cross_section_KCHS_TXKF_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/01\/190123_18utc_gfs90_cross_section_KCHS_TXKF_anim.gif\" alt=\"Cross sections of GFS90 model fields along Line I-I', from Charleston, South Carolina to Bermuda [click to enlarge]\" width=\"641\" height=\"370\" \/><\/a><p class=\"wp-caption-text\">Cross sections of GFS90 model fields along Line I-I&#8217;, from Charleston, South Carolina to Bermuda [click to enlarge]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>With a ridge of high pressure in place over the western Atlantic Ocean, GOES-16 (GOES-East) Mid-level Water Vapor (6.9 \u00b5m) images (above) indicated the presence of dry air within the middle troposphere off the Southeast US coast on 23 January 2019. GOES-16 &#8220;Red&#8221; Visible (0.64 \u00b5m) images showed that marine boundary layer stratocumulus clouds covered [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":31461,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[74,12,71],"tags":[],"class_list":["post-31455","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-16","category-modis","category-terra"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/31455","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=31455"}],"version-history":[{"count":10,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/31455\/revisions"}],"predecessor-version":[{"id":31470,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/31455\/revisions\/31470"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/31461"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=31455"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=31455"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=31455"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}