{"id":53549,"date":"2023-07-20T09:13:00","date_gmt":"2023-07-20T09:13:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=53549"},"modified":"2023-07-20T19:10:16","modified_gmt":"2023-07-20T19:10:16","slug":"tropical-storm-calvin-moves-through-the-hawaiian-islands","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/53549","title":{"rendered":"Tropical Storm Calvin moves through the Hawai&#8217;ian Islands"},"content":{"rendered":"\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/07\/G18NightMicro-20230719_0921_to_1321anim.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"1715\" height=\"969\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/07\/G18NightMicro-20230719_0921_to_1321anim.gif\" alt=\"\" class=\"wp-image-53554\"\/><\/a><figcaption class=\"wp-element-caption\">GOES-18 Night Microphysics RGB, 0921-1321 UTC on 19 July 2023 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>GOES-18 Night Microphysics imagery from 19 July 2023, above, shows a disorganized Tropical Storm Calvin moving south of Hawai&#8217;i before sunrise on 19 July.  The low-level swirl of the system is apparent to the south of the Big Island; convection associated with the system develops during the animation over Hawai&#8217;i, and high clouds with the system are present to the east of Hawai&#8217;i.  Convection produced heavy rains that closed some roads.  The CPHC discussion on the storm at 1500 UTC (<a href=\"https:\/\/www.nhc.noaa.gov\/archive\/2023\/ep03\/ep032023.discus.032.shtml?\">link<\/a>) noted the separation between the surface and mid- and upper-level features.  Visible imagery, below, a bit later than the animation above, shows the obvious low-level swirl (still associated with occasional isolated convection), but by <a href=\"https:\/\/www.nhc.noaa.gov\/archive\/2023\/ep03\/ep032023.discus.033.shtml?\">2100 UTC<\/a>, the system was declared post-tropical.<\/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\/2023\/07\/G18Band02-20230719_16336_to_2041anim.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"1040\" height=\"907\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/07\/G18Band02-20230719_16336_to_2041anim.gif\" alt=\"\" class=\"wp-image-53556\"\/><\/a><figcaption class=\"wp-element-caption\">GOES-18 Visible Imagery (Band 2, 0.64 \u00b5m), 1636-2041 UTC on 19 July 2023 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>By 0800 UTC on 20 July 2023, the system had weakened to an open-wave as shown in the Advanced Scatterometer (ASCAT) image shown below from <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/07\/MetopCPath_20July2023_HONOLULU.gif\">Metop-C<\/a>.  Winds of 30-35 knots are still indicated, but no westerly winds Equatorward of the strong easterly winds are present.<\/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\/2023\/07\/MetopC_ASCAT_20July2023.png\"><img loading=\"lazy\" decoding=\"async\" width=\"740\" height=\"650\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/07\/MetopC_ASCAT_20July2023.png\" alt=\"\" class=\"wp-image-53550\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/07\/MetopC_ASCAT_20July2023.png 740w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/07\/MetopC_ASCAT_20July2023-300x264.png 300w\" sizes=\"auto, (max-width: 740px) 100vw, 740px\" \/><\/a><figcaption class=\"wp-element-caption\">Metop-C Advanced Scatterometer (ASCAT) winds, 0820 UTC on 20 July 2023 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<p>Calvin brought extraordinary moisture to the Hawai&#8217;ian islands.  The 1200 UTC sounding at Hilo, below, (also available <a href=\"https:\/\/weather.uwyo.edu\/cgi-bin\/sounding?region=naconf&amp;TYPE=GIF%3ASKEWT&amp;YEAR=2023&amp;MONTH=07&amp;FROM=1912&amp;TO=1912&amp;STNM=91285\">here<\/a>) showed Total Precipitable Water exceeding 2.5&#8243;!  That value, if verified, means this is one of the top 5 wettest soundings at that location according to the <a href=\"https:\/\/www.spc.noaa.gov\/exper\/soundingclimov2\/\">SPC Sounding Climatology site<\/a>.  <a href=\"http:\/\/tropic.ssec.wisc.edu\/real-time\/mtpw2\/product.php?color_type=tpw_nrl_colors&amp;prod=epac&amp;timespan=24hrs&amp;anim=html5\">MIMIC Total Precipitable Water<\/a> values, shown at bottom in the animation from 0000 UTC 19 July to 0000 UTC 20 July, show the moisture associated with the storm.<\/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\/2023\/07\/PHTOSkewT_1200_19July2023.png\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"748\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/07\/PHTOSkewT_1200_19July2023-1024x748.png\" alt=\"\" class=\"wp-image-53557\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/07\/PHTOSkewT_1200_19July2023-1024x748.png 1024w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/07\/PHTOSkewT_1200_19July2023-300x219.png 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/07\/PHTOSkewT_1200_19July2023-768x561.png 768w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/07\/PHTOSkewT_1200_19July2023.png 1335w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a><figcaption class=\"wp-element-caption\">SkewT representation of upper air rawinsonde at Hilo, HI, 1200 UTC on 19 July 2023 (Click to enlarge)<\/figcaption><\/figure>\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\/2023\/07\/comp20230719.0000_to_0720_0000_tpw_anim.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"1000\" height=\"470\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/07\/comp20230719.0000_to_0720_0000_tpw_anim.gif\" alt=\"\" class=\"wp-image-53559\"\/><\/a><figcaption class=\"wp-element-caption\">MIMIC TPW fields 0000 UTC 19 July &#8212; 0000 UTC 20 July 2023 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<p>The identification of the low-level circulation at night in this case was not difficult, perhaps because high clouds were not present over the low-level circulation.  The toggle below shows Night Microphysics and the Day Night Band visible image (the New Moon occurred on 17 July, so very little lunar illumination was present).  The low-level swirl is apparent in both images.<\/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\/2023\/07\/G18NightMicroN20DNB-20230719_1221toggle.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"1715\" height=\"969\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/07\/G18NightMicroN20DNB-20230719_1221toggle.gif\" alt=\"\" class=\"wp-image-53563\"\/><\/a><figcaption class=\"wp-element-caption\">GOES-18 Night Microphysics RGB, 1221 UTC, and NOAA-20 Day Night Band visible (0.7 \u00b5m)  imagery, 1221 UTC on 19 July 2023 (click to enlarge)<\/figcaption><\/figure>\n","protected":false},"excerpt":{"rendered":"<p>GOES-18 Night Microphysics imagery from 19 July 2023, above, shows a disorganized Tropical Storm Calvin moving south of Hawai&#8217;i before sunrise on 19 July. The low-level swirl of the system is apparent to the south of the Big Island; convection associated with the system develops during the animation over Hawai&#8217;i, and high clouds with the [&hellip;]<\/p>\n","protected":false},"author":19,"featured_media":53561,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[114,78,25,2,48],"tags":[],"class_list":["post-53549","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-18","category-noaa-20","category-satellite-winds","category-tropical-cyclones","category-viirs"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/53549","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=53549"}],"version-history":[{"count":4,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/53549\/revisions"}],"predecessor-version":[{"id":53571,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/53549\/revisions\/53571"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/53561"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=53549"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=53549"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=53549"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}