{"id":36387,"date":"2020-04-24T23:59:17","date_gmt":"2020-04-24T23:59:17","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=36387"},"modified":"2020-04-25T23:53:23","modified_gmt":"2020-04-25T23:53:23","slug":"tropical-invest-90e-in-the-east-pacific-ocean","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/36387","title":{"rendered":"Tropical Depression One-E forms in the East Pacific Ocean"},"content":{"rendered":"<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200424_goes17_visible_infrared_East_Pacific_Invest90E_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/pac_vis-20200424_191025.png\" alt=\"GOES-17 \u201cRed\u201d Visible (0.64 \u00b5m) and \u201cClean\u201d Infrared Window (10.35 \u00b5m) images [click to play animation | MP4] \" width=\"641\" height=\"299\" \/><\/a><p class=\"wp-caption-text\">GOES-17 \u201cRed\u201d Visible<em> (0.64 \u00b5m)<\/em> and \u201cClean\u201d Infrared Window <em>(10.35 \u00b5m)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200424_goes17_visible_infrared_East_Pacific_Invest90E_anim.mp4\"><strong>MP4]<\/strong><\/a><\/p><\/div>1-minute <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/23225\"><strong>Mesoscale Domain Sector<\/strong><\/a> GOES-17 <em>(GOES-West)<\/em> \u201cRed\u201d Visible (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band02.pdf\"><strong>0.64 \u00b5m<\/strong><\/a>) and \u201cClean\u201d Infrared Window (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band13.pdf\"><strong>10.35 \u00b5m<\/strong><\/a>) images <strong>(above)<\/strong> showed the circulation of Tropical Invest 90E in the East Pacific Ocean on 24 April 2020. The low-level circulation center appeared to be located about 100 miles southwest of the 18 UTC surface analysis position.<\/p>\n<p>GOES-17 Visible images with a plot of <a href=\"http:\/\/tropic.ssec.wisc.edu\/misc\/winds\/info.winds.shr.html\"><strong>Deep-Layer Wind Shear<\/strong><\/a> from the <a href=\"http:\/\/tropic.ssec.wisc.edu\/\"><strong>CIMSS Tropical Cyclones<\/strong><\/a> site <em><strong>(below)<\/strong><\/em> indicated that Invest 90E was embedded within an environment of low shear &#8212; the National Hurricane Center gave the feature an <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200424_two_Invest90E.png\"><strong>80% chance<\/strong><\/a> of further developing into a tropical depression within 48 hours.<\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200424_23utc_goes17_visible_shear_Invest90E_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200424_23utc_goes17_visible_shear_Invest90E_anim.gif\" alt=\"GOES-17 \u201cRed\u201d Visible (0.64 \u00b5m) with a plot of Deep-Layer Wind Shear at 23 UTC images [click to enlarge]\" width=\"641\" height=\"428\" \/><\/a><p class=\"wp-caption-text\">GOES-17 \u201cRed\u201d Visible<em> (0.64 \u00b5m)<\/em> images, with a plot of Deep-Layer Wind Shear at 23 UTC [click to enlarge]<\/p><\/div>VIIRS True Color RGB and Infrared Window (11.45 \u00b5m) images from NOAA-20 and Suomi NPP as viewed using <a href=\"http:\/\/realearth.ssec.wisc.edu\"><strong>RealEarth<\/strong><\/a><em><strong> (below)<\/strong><\/em> revealed tendrils of transverse banding along the western and northern periphery if the disturbance.<\/p>\n<div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200424_noaa20_suomiNPP_trueColorRGB_infraredWindow_East_Pacific_Invest90E_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200424_noaa20_suomiNPP_trueColorRGB_infraredWindow_East_Pacific_Invest90E_anim.gif\" alt=\"VIIRS True Color RGB and Infrared Window (11.45 \u00b5m) images from NOAA-20 and Suomi NPP [click to enlarge]\" width=\"641\" height=\"335\" \/><\/a><p class=\"wp-caption-text\">VIIRS True Color RGB and Infrared Window <em>(11.45 \u00b5m)<\/em> images from NOAA-20 and Suomi NPP [click to enlarge]<\/p><\/div>\n<p style=\"text-align: center;\"><strong>===== 25 April Update =====<\/strong><\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200425_goes17_infrared_Tropical_Depression_One_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/G17_IR_TD_ONE_25APR2020_B13_2020116_150032_GOES-17_0001PANEL_FRAME00032.GIF\" alt=\"GOES-17 \u201cClean\u201d Infrared Window (10.35 \u00b5m) images [click to play animation | MP4]\" width=\"641\" height=\"481\" \/><\/a><p class=\"wp-caption-text\">GOES-17 \u201cClean\u201d Infrared Window <em>(10.35 \u00b5m)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200425_goes17_infrared_Tropical_Depression_One_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>GOES-17 Infrared images <em><strong>(above)<\/strong> <\/em>showed the period when the disturbance became classified as Tropical Depression One-E at <a href=\"https:\/\/www.nhc.noaa.gov\/text\/refresh\/MIATCDEP1+shtml\/251448.shtml?\"><strong>15 UTC<\/strong><\/a> &#8212; making this the earliest tropical cyclone on record in the East Pacific basin during the satellite era.<\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200425_goes17_infrared_surfaceAnalysis_TD_One_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/pac_ir-20200425_120032.png\" alt=\"GOES-17 \u201cClean\u201d Infrared Window (10.35 \u00b5m) images [click to play animation | MP4]\" width=\"641\" height=\"299\" \/><\/a><p class=\"wp-caption-text\">GOES-17 \u201cClean\u201d Infrared Window<em> (10.35 \u00b5m)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200425_goes17_infrared_surfaceAnalysis_TD_One_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>GOES-17 Infrared images with plots of tropical surface analyses <em><strong>(above)<\/strong><\/em> indicated that TD One-E was situated just north of the Intertropical Convergence Zone (<a href=\"https:\/\/en.wikipedia.org\/wiki\/Intertropical_Convergence_Zone\"><strong>ITCZ<\/strong><\/a>). The <a href=\"http:\/\/tropic.ssec.wisc.edu\/real-time\/mtpw2\/product.php?color_type=tpw_nrl_colors&amp;prod=global2&amp;timespan=24hrs&amp;anim=html5\"><strong>MIMIC-TPW<\/strong><\/a> product<em><strong> (below)<\/strong><\/em> showed that the tropical depression was tapping moisture from the ITCZ and drawing it northward.<\/p>\n<p><div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200424_200425_mimicTPW_East_Pacific_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200424_200425_mimicTPW_East_Pacific_anim.gif\" alt=\"MIMIC Total Precipitable Water product [click to enlarge]\" width=\"642\" height=\"302\" \/><\/a><p class=\"wp-caption-text\">MIMIC Total Precipitable Water product [click to enlarge]<\/p><\/div>GOES-17 Visible images <em><strong>(below)<\/strong><\/em> revealed an exposed low-level circulation that was displaced north-northwest of the primary cluster of deep convection.<\/p>\n<div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200425_goes17_visible_Tropical_Depression_One_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/G17_VIS_TD_ONE_25APR2020_B2_2020116_150032_GOES-17_0001PANEL_FRAME00009.GIF\" alt=\"GOES-17 \u201cRed\u201d Visible (0.64 \u00b5m) images [click to play animation | MP4]\" width=\"641\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">GOES-17 \u201cRed\u201d Visible<em> (0.64 \u00b5m)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200425_goes17_visible_Tropical_Depression_One_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>1-minute Mesoscale Domain Sector GOES-17 (GOES-West) \u201cRed\u201d Visible (0.64 \u00b5m) and \u201cClean\u201d Infrared Window (10.35 \u00b5m) images (above) showed the circulation of Tropical Invest 90E in the East Pacific Ocean on 24 April 2020. The low-level circulation center appeared to be located about 100 miles southwest of the 18 UTC surface analysis position. GOES-17 Visible [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":36391,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[80,79,78,53,45,25,49,2,48],"tags":[],"class_list":["post-36387","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-17","category-microwave","category-noaa-20","category-real-earth","category-redgreenblue-rgb-images","category-satellite-winds","category-suomi_npp","category-tropical-cyclones","category-viirs"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/36387","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=36387"}],"version-history":[{"count":9,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/36387\/revisions"}],"predecessor-version":[{"id":36397,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/36387\/revisions\/36397"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/36391"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=36387"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=36387"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=36387"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}