{"id":32608,"date":"2019-03-26T23:59:57","date_gmt":"2019-03-26T23:59:57","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=32608"},"modified":"2019-03-29T17:03:13","modified_gmt":"2019-03-29T17:03:13","slug":"strong-cyclone-near-antarctica","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/32608","title":{"rendered":"Strong cyclone near Antarctica"},"content":{"rendered":"<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/190325_infrared_composite_Antarctica_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/190326_19z_ant.GIF\" alt=\"Composites of geostationary and polar orbiter Infrared imagery [click to play animation]\" width=\"640\" height=\"648\" \/><\/a><p class=\"wp-caption-text\">Composites of geostationary and polar orbiter <strong>Infrared<\/strong> imagery [click to play animation]<\/p><\/div>Composites of Infrared imagery <em><strong>(above)<\/strong><\/em> and Water Vapor imagery<em><strong> (below)<\/strong><\/em> from the <a href=\"https:\/\/amrc.ssec.wisc.edu\/data\/view-data.php?action=list&amp;product=satellite\/composite\"><strong>AMRC<\/strong><\/a> site showed an anomalously strong (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/190326_mslp_anomaly_South_Pacific_anim.gif\"><strong>MSLP<\/strong><\/a> | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/190326_925hPa_wind_anomaly_South_Pacific_anim.gif\"><strong>925 hPa winds<\/strong><\/a> | <a href=\"http:\/\/www.atmos.albany.edu\/student\/abentley\/realtime.html\"><strong>source<\/strong><\/a>) cyclone that was moving southeastward across the South Pacific Ocean toward the coast of Antarctica on 26 March 2019. These composites blend images from both geostationary and polar orbiting satellites; the storm is located in the upper right quadrant of the images. On the Infrared imagery, brighter white shades over much of the middle of Antarctica indicated a very cold surface &#8212; in fact, <strong><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/190326_23z_aws_temp.GIF\">surface air temperatures<\/a><\/strong> were as cold as -84\u00baF over the interior of the continent at 23 UTC.<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/190325_waterVapor_composite_Antarctica_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/190326_19z_wv_ant.GIF\" alt=\"Composites of geostationary and polar orbiter Water Vapor imagery [click to play animation]\" width=\"640\" height=\"647\" \/><\/a><p class=\"wp-caption-text\">Composites of geostationary and polar orbiter <strong>Water Vapor<\/strong> imagery [click to play animation]<\/p><\/div>The storm was evident along the southern limb of GOES-16 Full Disk scans, as seen on Mid-level Water Vapor (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band09.pdf\"><strong>6.9 \u00b5m<\/strong><\/a>) and &#8220;Red&#8221; Visible (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band02.pdf\"><strong>0.64 \u00b5m<\/strong><\/a>) images <em><strong>(below)<\/strong><\/em>. The location of AMRC <a href=\"https:\/\/amrc.ssec.wisc.edu\/aws\/index.php?region=All%20Stations&amp;mode=international\"><strong>AWS<\/strong><\/a> station <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/Thurston_Island_AWS.png\"><strong>8930 (Thurston Island)<\/strong><\/a> near the coast of <a href=\"https:\/\/upload.wikimedia.org\/wikipedia\/commons\/c\/c0\/Antarctica.svg\"><strong>Ellsworth Land<\/strong><\/a> in West Antarctica is indicated in red.<\/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\/03\/190325_goes16_waterVapor_South_Pacific_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/G16_WV_ANTARCTICA_26MAR2019_2019085_120036_GOES-16_0001PANEL.GIF\" alt=\"GOES-16 Mid-level Water Vapor images [click to play animation | MP4]\" width=\"639\" height=\"323\" \/><\/a><p class=\"wp-caption-text\">GOES-16 Mid-level Water Vapor <em>(6.9 \u00b5m)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/190325_goes16_waterVapor_South_Pacific_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div><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\/03\/190325_goes16_visible_South_Pacific_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/G16_VIS_ANTARCTICA_26MAR2019_2019085_180034_GOES-16_0001PANEL.GIF\" alt=\"GOES-16 &quot;Red&quot; Visible (0.64 \u00b5m) images [click to play animation | MP4]\" width=\"639\" height=\"323\" \/><\/a><p class=\"wp-caption-text\">GOES-16 &#8220;Red&#8221; Visible <em>(0.64 \u00b5m)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/190325_goes16_visible_South_Pacific_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>This storm was also evident at the bottom center of a GOES-17 + GOES-16 composite of north-to-south True Color Red-Green-Blue (RGB) swaths of 15-minute illumination at local solar noon &#8212; beginning at 12 UTC in the east, and ending at 03 UTC in the west &#8212; combined and displayed in a Mollweide projection<em><strong> (below<\/strong>; courtesy of Rick Kohrs, SSEC)<\/em>.<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/g16-g17-noon-composite-2019086.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/g16-g17-noon-composite-2019086.jpg\" alt=\"GOES-17 + GOES-16 True Color RGB image [click to enlarge]\" width=\"640\" height=\"503\" \/><\/a><p class=\"wp-caption-text\">GOES-17 + GOES-16 True Color RGB image [click to enlarge]<\/p><\/div>A time series of surface observation data from AWS station 8930 on Thurston Island <em><strong>(below)<\/strong><\/em> showed that southeasterly winds peaked at 113 knots (58 m\/s) late in the day on 26 March as the strong low pressure system approached. According to AMRC staff, this particular AWS is located on a nunatak near Parker Peak in the Walker Mountains (<a href=\"https:\/\/en.wikipedia.org\/wiki\/Thurston_Island#\/media\/File:Thurston_Island_-_en.svg\"><strong>map<\/strong><\/a>) &#8212; such an exposure is prone to periods of strong winds, requiring a recent retrofitting of special instrumentation designed to withstand and measure higher wind speeds.<\/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\/03\/190327_15z_8930_Thurston_Island_sfcmg_ant.GIF\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/190327_15z_8930_Thurston_Island_sfcmg_ant.GIF\" alt=\"Tiime series of surface observation data from AWS station 8930 Thurston Island [click to enlarge]\" width=\"641\" height=\"641\" \/><\/a><p class=\"wp-caption-text\">Time series of surface observation data from AWS station 8930 Thurston Island [click to enlarge]<\/p><\/div>A closer look with GOES-16 Visible and Low-level Water Vapor (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band10.pdf\"><strong>7.3 \u00b5m<\/strong><\/a>) images <em><strong>(below)<\/strong><\/em> revealed small wave perturbations in the cloud field and the eventual formation of a banner cloud as <a href=\"https:\/\/en.wikipedia.org\/wiki\/Peter_I_Island\"><strong>Peter I Island<\/strong><\/a> was acting as an obstacle to the strong boundary layer winds south of the storm center.<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/190326_goes16_visible_waterVapor_Peter_Island_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/190326_1500utc_goes16_visible_waterVapor_Peter_I_Island.png\" alt=\"GOES-16 &quot;Red&quot; Visible (0.64 \u00b5m. left) and Low-level Water Vapor (7.3 \u00b5m, right) images [click to play animation | MP4]\" width=\"640\" height=\"482\" \/><\/a><p class=\"wp-caption-text\">GOES-16 &#8220;Red&#8221; Visible <em>(0.64 \u00b5m. left)<\/em> and Low-level Water Vapor <em>(7.3 \u00b5m, right)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/190326_goes16_visible_waterVapor_Peter_Island_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>A timely overpass of the Landsat-8 satellite provided a 30-meter resolution Landsat-8 False Color RGB image, viewed using <a href=\"http:\/\/realearth.ssec.wisc.edu\"><strong>RealEarth<\/strong><\/a> <em><strong>(below)<\/strong>,<\/em> of these orographically-induced cloud perturbations.<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/190326_1456utc_landsat8_falsecolor_Peter_I_Island_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/190326_1456utc_landsat8_falsecolor_Peter_I_Island_anim.gif\" alt=\"Landsat-8 False Color image [click to enlarge]\" width=\"640\" height=\"374\" \/><\/a><p class=\"wp-caption-text\">Landsat-8 False Color RGB image [click to enlarge]<\/p><\/div>The orographic wave clouds downwind of Peter I Island could also be seen on 375-meter resolution Suomi NPP VIIRS True Color RGB and Infrared Window (11.45 \u00b5m) images at 19 UTC and 21 UTC <em><strong>(below)<\/strong><\/em>.<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/190326_suomiNPP_viirs_truecolor_infraredWindow_South_Pacific_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/190326_suomiNPP_viirs_truecolor_infraredWindow_South_Pacific_anim.gif\" alt=\"Suomi NPP VIIRS True Color RGB and Infrared Window (11.45 \u00b5m) images 1t 19 UTC and 21 UTC [click to enlarge]\" width=\"640\" height=\"374\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS True Color RGB and Infrared Window<em> (11.45 \u00b5m)<\/em> images at 19 UTC and 21 UTC [click to enlarge]<\/p><\/div><center><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p dir=\"ltr\" lang=\"en\"><a href=\"https:\/\/twitter.com\/hashtag\/GOESWest?src=hash&amp;ref_src=twsrc%5Etfw\">#GOESWest<\/a> is watching a hurricane-force low that&#8217;s headed toward the Antarctic Peninsula. This loop uses what&#8217;s known as Air Mass RGB Imagery, which helps distinguish polar from tropical air masses. More imagery: <a href=\"https:\/\/t.co\/3SWkPqjxr9\">https:\/\/t.co\/3SWkPqjxr9<\/a> <a href=\"https:\/\/t.co\/nUOKrYtfm1\">pic.twitter.com\/nUOKrYtfm1<\/a><\/p>\n<p>\u2014 NOAA Satellites (@NOAASatellites) <a href=\"https:\/\/twitter.com\/NOAASatellites\/status\/1110630292941877248?ref_src=twsrc%5Etfw\">March 26, 2019<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><br \/>\n<\/center><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Composites of Infrared imagery (above) and Water Vapor imagery (below) from the AMRC site showed an anomalously strong (MSLP | 925 hPa winds | source) cyclone that was moving southeastward across the South Pacific Ocean toward the coast of Antarctica on 26 March 2019. These composites blend images from both geostationary and polar orbiting satellites; [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":32614,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[36,74,80,55,53,45,49,48],"tags":[],"class_list":["post-32608","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-antarctic","category-goes-16","category-goes-17","category-landsat","category-real-earth","category-redgreenblue-rgb-images","category-suomi_npp","category-viirs"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/32608","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=32608"}],"version-history":[{"count":23,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/32608\/revisions"}],"predecessor-version":[{"id":32637,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/32608\/revisions\/32637"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/32614"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=32608"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=32608"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=32608"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}