{"id":56178,"date":"2023-12-24T12:59:00","date_gmt":"2023-12-24T12:59:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=56178"},"modified":"2023-12-26T04:22:27","modified_gmt":"2023-12-26T04:22:27","slug":"hurricane-force-low-in-the-gulf-of-alaska","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/56178","title":{"rendered":"Hurricane Force Low in the Gulf of Alaska"},"content":{"rendered":"<p><div style=\"width: 1725px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231223_goes18_airMassRGB_pv1.5pressure_Gulf_of_Alaska_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/ak_rgb-20231224_000022.png\" width=\"1715\" height=\"830\" \/><\/a><p class=\"wp-caption-text\">GOES-18 Air Mass RGB images, with\/without contours of AK-NAM40 model PV 1.5 Pressure, from 0000 UTC on 23 December to 0300 UTC on 24 December [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231223_goes18_airMassRGB_pv1.5pressure_Gulf_of_Alaska_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>10-minute Full Disk scan GOES-18 <a href=\"https:\/\/rammb2.cira.colostate.edu\/wp-content\/uploads\/2020\/01\/QuickGuide_GOESR_AirMassRGB_final-1.pdf\"><strong>Air Mass RGB<\/strong><\/a> images <em><strong>(above)<\/strong><\/em> showed a cyclone as it intensified to a Hurricane Force Low by 0000 UTC on 24 December 2023 as it moved north across the Gulf of Alaska (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231223_231224_AK_surface_analyses_anim.gif\"><strong>suface analyses<\/strong><\/a>). Brighter orange-red hues in the RGB images highlighted a Potential Vortcity (PV) Anomaly within the core of the low pressure system &#8212; AK-NAM40 model fields indicated that the &#8220;dynamic tropopause&#8221; (taken to be the pressure of the PV 1.5 surface) had descended to near the 800 hPa pressure level at 0000 UTC on 24 December <em><strong>(below)<\/strong><\/em>.<\/p>\n<p><div style=\"width: 1725px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/2312234_0000utc_goes18_airMassRGB_pv1.5pressure_Gulf_of_Alaska_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/2312234_0000utc_goes18_airMassRGB_pv1.5pressure_Gulf_of_Alaska_anim.gif\" width=\"1715\" height=\"830\" \/><\/a><p class=\"wp-caption-text\">GOES-18 Air Mass RGB image at 0000 UTC on 24 December, with\/without contours of AK-NAM40 model PV 1.5 Pressure [click to enlarge]<\/p><\/div>A closer view of GOES-18 Air Mass RGB and 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>(below)<\/strong><\/em> displayed the low as it eventually moved inland across Southcentral Alaska by 1200 UTC on 24 December. Notable peak wind gusts included 70 knots at <a href=\"https:\/\/www.ndbc.noaa.gov\/station_page.php?station=46082\"><strong>Buoy 46082<\/strong><\/a> at <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231225_%20buoy46082_wind_pressure.png\"><strong>0710 UTC<\/strong><\/a>, 69 knots at Middleton Island (PAMD) around <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/ak_wv_zoom-20231224_020022.png\"><strong>0200 UTC<\/strong><\/a> and 60 knots at Codova (PACV) around <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/ak_wv_zoom-20231224_110022.png\"><strong>1100 UTC<\/strong><\/a>.<\/p>\n<p><div style=\"width: 1725px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231223_231224_goes18_airMassRGB_waterVapor_surfaceReports_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/ak_wv_zoom-20231224_020022.png\" width=\"1715\" height=\"830\" \/><\/a><p class=\"wp-caption-text\">GOES-18 Air Mass RGB and Mid-level Water Vapor (6.9 \u00b5m) images, with plots of Surface\/Buoy\/Ship Reports, from 0000 UTC to 1200 UTC on 24 December [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231223_231224_goes18_airMassRGB_waterVapor_surfaceReports_AK_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>This Hurricane Force Low was rather anomalous in terms of its low Mean Sea Level Pressure (MSLP) and strong 925 hPa wind speeds (<a href=\"https:\/\/www.atmos.albany.edu\/student\/abentley\/realtime.html\"><strong>source<\/strong><\/a>), as shown below.<\/p>\n<div style=\"width: 1170px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231223_231224_meanSeaLevelPressure_anomaly_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231223_231224_meanSeaLevelPressure_anomaly_anim.gif\" width=\"1160\" height=\"914\" \/><\/a><p class=\"wp-caption-text\">MSLP Anomaly [click to enlarge]<\/p><\/div>\n<div style=\"width: 1170px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231223_231224_925ha_wind_speed_anomaly_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231223_231224_925ha_wind_speed_anomaly_anim.gif\" width=\"1160\" height=\"914\" \/><\/a><p class=\"wp-caption-text\">925 hPa Wind Speed anomaly [click to enlarge]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>10-minute Full Disk scan GOES-18 Air Mass RGB images (above) showed a cyclone as it intensified to a Hurricane Force Low by 0000 UTC on 24 December 2023 as it moved north across the Gulf of Alaska (suface analyses). Brighter orange-red hues in the RGB images highlighted a Potential Vortcity (PV) Anomaly within the core [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":56182,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[114,45],"tags":[],"class_list":["post-56178","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-18","category-redgreenblue-rgb-images"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/56178","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=56178"}],"version-history":[{"count":5,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/56178\/revisions"}],"predecessor-version":[{"id":56185,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/56178\/revisions\/56185"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/56182"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=56178"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=56178"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=56178"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}