{"id":68617,"date":"2026-01-24T23:59:00","date_gmt":"2026-01-24T23:59:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=68617"},"modified":"2026-02-06T19:14:57","modified_gmt":"2026-02-06T19:14:57","slug":"thunderstorms-prompt-the-issuance-of-flash-flood-warnings-in-american-samoa","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/68617","title":{"rendered":"Thunderstorms prompt the issuance of Flash Flood Warnings in American Samoa"},"content":{"rendered":"<p><div style=\"width: 3258px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/01\/260124_goes18_infrared_glmFlashPoints_American_Samoa.mp4\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/01\/260124_1850utc_g18_glm.png\" width=\"3248\" height=\"1912\" \/><\/a><p class=\"wp-caption-text\">1-minute GOES-18 Infrared images with an overlay of GLM Flash Points (white dots) and METAR surface reports (cyan), from 1501 UTC on 24 January to 0000 UTC on 25 January [click to play MP4 animation]<\/p><\/div>Due to a lack of radar coverage over American Samoa, <a href=\"https:\/\/www.weather.gov\/ppg\/?lang=english\"><strong>WSO Pago Pago<\/strong><\/a> requested a 1-minute <a href=\"https:\/\/www.nco.ncep.noaa.gov\/status\/satellite\/\"><strong>Mesoscale Domain Sector<\/strong><\/a> over the islands to monitor convective development and the potential for flash flooding. GOES-18 <em>(GOES-West)<\/em>\u00a0Clean Infrared Window (10.3 \u00b5m) images <em><strong>(above)<\/strong><\/em>\u00a0showed rain showers and thunderstorms that developed in the general vicinity of the American Samoa island of Tutuila (where Pago Pago International Airport NSTU is located) on 24 January 2026. <a href=\"https:\/\/www.goes-r.gov\/spacesegment\/glm.html\"><strong>GLM<\/strong><\/a> Flash Points indicated that intermittent lightning occurred near Tutuila \u2014 and thunderstorms were occasionally reported at NSTU. The development of deep convection was enhanced by the presence of a surface trough of low pressure across the area (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/01\/260124_15z_sfc_fj.jpg\"><strong>1500 UTC<\/strong><\/a> | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/01\/260124_18z_sfc_fj.jpg\"><strong>1800 UTC<\/strong><\/a> | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/01\/260125_00z_sfc_fj.jpg\"><strong>0000 UTC<\/strong><\/a>).<\/p>\n<p>The coldest cloud-top infrared brightness temperatures were in the -85 to -89\u00baC range (darker shades of purple embedded within brighter white regions) &#8212; which represented a slight overshoot of the Most Unstable (MU) air parcel&#8217;s Equilibrium Level (EL), which was around 15 km (or 50 kft) according to a plot of rawinsonde data from NSTU at 0000 UTC on 25 January <em><strong>(below)<\/strong><\/em>.<\/p>\n<p><div style=\"width: 2992px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/01\/260125_0000utc_nstu_raob.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/01\/260125_0000utc_nstu_raob.png\" width=\"2982\" height=\"1662\" \/><\/a><p class=\"wp-caption-text\">Plot of rawinsonde data from Pago Pago, American Samoa at 0000 UTC on 25 January [click to enlarge]<\/p><\/div>The GOES-18 Infrared image at 1850 UTC <em><strong>(below)<\/strong><\/em> included a sample of the corresponding NSTU METAR &#8212; which indicated that a thunderstorm with heavy rain showers was reducing the visibility to 3 miles at that time. Note that the coldest cloud-top infrared brightness temperatures of that particular thunderstorm (violet pixels) were displaced to the <em>southwest<\/em> of NSTU, due to a GOES-West\u00a0<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/webapps\/parallax\/overview.html\"><strong>parallax<\/strong><\/a> offset associated with a cloud-top altitude around <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/06\/parallax_goes18_50kft_American_Samoa.png\"><strong>50 kft or 15.2 km<\/strong><\/a>.<\/p>\n<p><div style=\"width: 2992px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/01\/260124_1850utc_goes18_infrared_nstu_metar.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/01\/260124_1850utc_goes18_infrared_nstu_metar.png\" width=\"2982\" height=\"1662\" \/><\/a><p class=\"wp-caption-text\">GOES-18 Infrared image at 1850 UTC on 24 January, with a cursor sample of the 1850 UTC Pago Pago (NSTU) METAR surface report [click to enlarge]<\/p><\/div>The GOES-18 Infrared image at 2058 UTC <em><strong>(below)<\/strong><\/em> included a sample of the corresponding NSTU METAR &#8212; which indicated that a thunderstorm had earlier occurred from 1800-1856 UTC, and heavy rain showers had occurred from 1811-1951 UTC.<\/p>\n<div style=\"width: 3034px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/01\/260124_2058utc_goes18_infrared_nstu_metar.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/01\/260124_2058utc_goes18_infrared_nstu_metar.png\" width=\"3024\" height=\"1964\" \/><\/a><p class=\"wp-caption-text\">GOES-18 Infrared image at 2058 UTC on 24 January, with a cursor sample of the 2058 UTC Pago Pago (NSTU) METAR surface report [click to enlarge]<\/p><\/div>\n<p style=\"text-align: center;\">________________________<\/p>\n<p><div style=\"width: 3150px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/01\/260124_nstu_decoded_observations.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/01\/260124_nstu_decoded_observations.png\" width=\"3140\" height=\"2112\" \/><\/a><p class=\"wp-caption-text\">Decoded surface reports from Pago Pago, with the precipitation reports for 24 January (local time) highlighted by a green box [click to enlarge]<\/p><\/div>Pago Pago recorded 2.76&#8243; of rainfall during their calendar day of 24 January <em><strong>(above)<\/strong><\/em> &#8212; with most of that occurring during the ~2 hour period from 1811-1951 UTC <em><strong>(below)<\/strong><\/em>. WSO Pago Pago issued <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/01\/260124_ppg_ffw.text\"><strong>Flash Flood Warnings<\/strong><\/a> at 1812 UTC and 2100 UTC on 24 January.<\/p>\n<div style=\"width: 3150px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/01\/260124_nstu_metar.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/01\/260124_nstu_metar.png\" width=\"3140\" height=\"2112\" \/><\/a><p class=\"wp-caption-text\">Pago Pago METAR reports, with the period of heavy rain showers (+SHRA) occurring within the red box [click to enlarge]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>Due to a lack of radar coverage over American Samoa, WSO Pago Pago requested a 1-minute Mesoscale Domain Sector over the islands to monitor convective development and the potential for flash flooding. GOES-18 (GOES-West)\u00a0Clean Infrared Window (10.3 \u00b5m) images (above)\u00a0showed rain showers and thunderstorms that developed in the general vicinity of the American Samoa island [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":68621,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[76,114,16,30],"tags":[],"class_list":["post-68617","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-glm","category-goes-18","category-heavy-rain-flooding","category-lightning"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/68617","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=68617"}],"version-history":[{"count":23,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/68617\/revisions"}],"predecessor-version":[{"id":68833,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/68617\/revisions\/68833"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/68621"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=68617"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=68617"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=68617"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}