{"id":61175,"date":"2024-10-23T20:08:27","date_gmt":"2024-10-23T20:08:27","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=61175"},"modified":"2024-10-24T15:16:58","modified_gmt":"2024-10-24T15:16:58","slug":"the-samoan-islands-see-rain","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/61175","title":{"rendered":"The Samoan Islands see Rain"},"content":{"rendered":"\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"1000\" height=\"470\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/10\/comp20241022.0000_to_1300anim.gif\" alt=\"\" class=\"wp-image-61176\"\/><figcaption class=\"wp-element-caption\">MIMIC Total Precipitable Water fields, 0000-1300 UTC on 22 October 2024 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>MIMIC TPW fields for the first half of 22 October (at which point the data feed from NOAA\/NESDIS was interrupted) shows the Samoan Islands within an isolated region of relatively dry air with moisture moving in from the east. GFS fields showing the Galvez Davison Index (GDI) that is sometimes used to anticipate rain in the tropics, below (<a href=\"https:\/\/www.wpc.ncep.noaa.gov\/international\/gdi\/\">from this site<\/a>), shows a predicted increase in index values (suggesting an increase in rain probabilities;  GDI has been discussed on this Blog previously <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/48755\">here<\/a> and <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/48866\">here<\/a>).<\/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\/2024\/10\/GFSGDI_12zFCST_00-12h_23Oct2024stepanim2.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"1080\" height=\"740\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/10\/GFSGDI_12zFCST_00-12h_23Oct2024stepanim2.gif\" alt=\"\" class=\"wp-image-61182\"\/><\/a><figcaption class=\"wp-element-caption\">GFS estimates on Galvez-Davison Index, 1200 UTC 22 October &#8211; 0000 UTC 23 October 2024 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<p>Given this background, what might you examine to determine if rain is imminent?  Visible imagery from GOES-18 might be one example, as shown in the animation below from <a href=\"https:\/\/geosphere.ssec.wisc.edu\/#playing:true;coordinate:-3297760,-1488012;zoom:7.1;satellite:goeswest;product:%5B%7B%22n%22:%22c02%22,%22a%22:1%7D%5D;num_frames:38;start_time:2024-10-22T17:50:00Z;timeframe:Start%20Time;\">the CSPP-Geosphere site<\/a>.  Convective clouds approach the Samoan Islands from the east, coming very close to American Samoa but not overspreading the islands.  Convection does overspread Upolu by the end of the animation.<\/p>\n\n\n\n<figure class=\"wp-block-video\"><video height=\"1010\" style=\"aspect-ratio: 1284 \/ 1010;\" width=\"1284\" controls loop src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/10\/goeswest_abi_radf_c02_s20241022175021_e20241023000021_f38.mp4\"><\/video><figcaption class=\"wp-element-caption\">GOES-18 Visible Imagery (Band 2, 0.64 \u00b5m) 1750 UTC 22 October &#8211; 0000 UTC 23 October 2024<\/figcaption><\/figure>\n\n\n\n<p>GREMLIN is a product that predicts what radar would show given a distribution of GOES data (from bands 7, 9, and 13).  The animation below shows predicted radar echoes getting very close to Tutuila (the island including Pago Pago), and overspreading Upolu, the island of Samoa that includes its Capital city Apia.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"992\" height=\"823\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/10\/G18GREMLIN-20241022_1540_to_2210anim.gif\" alt=\"\" class=\"wp-image-61184\"\/><figcaption class=\"wp-element-caption\">GREMLIN estimates of radar echoes, 1540-2210 UTC on 22 October 2024 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>A meteorogram for Pago Pago, American Samoa (station NSTU) from 0300 UTC 22 October through 1500 UTC 23 October, below, shows that light rain was observed at Pago Pago airport at 22 UTC on 22 October. Heavier rain overspread the region on 23 October. A similar meteorogram for Apia, Samoa (station NSFA), follows, showing a similar tale, but does it show the rain that might have been expected (at Apia especially) given the imagery above?<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"768\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/10\/NSTU_METEOGRAM_22_23OCT2024-1024x768.gif\" alt=\"\" class=\"wp-image-61186\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/10\/NSTU_METEOGRAM_22_23OCT2024-1024x768.gif 1024w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/10\/NSTU_METEOGRAM_22_23OCT2024-300x225.gif 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/10\/NSTU_METEOGRAM_22_23OCT2024-768x576.gif 768w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><figcaption class=\"wp-element-caption\">Meteogram for Pago Pago, 0500 UTC 22 October &#8211; 1700 UTC 23 October 2024 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"768\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/10\/APIA_SAMOA_METEOGRAM_22_23OCT-1024x768.gif\" alt=\"\" class=\"wp-image-61188\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/10\/APIA_SAMOA_METEOGRAM_22_23OCT-1024x768.gif 1024w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/10\/APIA_SAMOA_METEOGRAM_22_23OCT-300x225.gif 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/10\/APIA_SAMOA_METEOGRAM_22_23OCT-768x576.gif 768w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><figcaption class=\"wp-element-caption\">Meteogram for Apia, Samoa, 0300 UTC 22 October &#8211; 1500 UTC 23 October 2024 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<p>Use large-scale products such as MIMIC or model fields of GDI to get a general feel for how precipitation might be approaching and\/or evolving, then examine satellite imagery, either individual bands or derived products, as <strong><span style=\"text-decoration: underline;\">guidance<\/span><\/strong> for your precipitation forecast in the short-term.<\/p>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<p class=\"has-text-align-center\">(Added, 24 October)<\/p>\n\n\n\n<p>You will note above that the meteorogram for Pago Pago shows rain starting at 1200 UTC on the 23rd.  What did the GREMLIN fields look like at that time?  The animation below spans 1100-1850 UTC on the 23rd.  GREMLIN gradually increases its estimations of radar echoes during this time, including the times in the meteorogram when rain was observed at NSTU.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"992\" height=\"823\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/10\/G18GREMLIN-20241023_1100_to_1850anim.gif\" alt=\"\" class=\"wp-image-61205\"\/><figcaption class=\"wp-element-caption\">GOES-18 GREMLIN fields, 1100-1850 UTC on 23 October 2024 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>The National Weather Service in Pago Pago used GREMLIN imagery (from <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/10\/G18GREMLIN-20241023_185021.png\">1850 UTC<\/a>) in the <a href=\"https:\/\/www.facebook.com\/NWSPagoPago\/posts\/pfbid037fqCQmuiEK291GuBHuY8HbjHtai5opuT9LZFJewEPV9zKvwHhX3cGP3guhtiT5oal\">Facebook post<\/a>, below, to alert their followers to the extent of the rain.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"682\" height=\"660\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/10\/NWAAmericanSamoaFBPost_0745PM23Oct.png\" alt=\"\" class=\"wp-image-61206\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/10\/NWAAmericanSamoaFBPost_0745PM23Oct.png 682w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/10\/NWAAmericanSamoaFBPost_0745PM23Oct-300x290.png 300w\" sizes=\"auto, (max-width: 682px) 100vw, 682px\" \/><figcaption class=\"wp-element-caption\">NWS Pago Pago Facebook post from 23 October 2024<\/figcaption><\/figure>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<p>GREMLIN fields are now available at the <a href=\"https:\/\/rammb-slider.cira.colostate.edu\/?sat=goes-18&amp;sec=full_disk&amp;x=10848&amp;y=10848&amp;z=0&amp;angle=0&amp;im=12&amp;ts=1&amp;st=0&amp;et=0&amp;speed=130&amp;motion=loop&amp;maps%5Bborders%5D=white&amp;p%5B0%5D=gremlin&amp;opacity%5B0%5D=1&amp;pause=0&amp;slider=-1&amp;hide_controls=0&amp;mouse_draw=0&amp;follow_feature=0&amp;follow_hide=0&amp;s=rammb-slider&amp;draw_color=FFD700&amp;draw_width=6\">CIRA SLIDER<\/a>.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>MIMIC TPW fields for the first half of 22 October (at which point the data feed from NOAA\/NESDIS was interrupted) shows the Samoan Islands within an isolated region of relatively dry air with moisture moving in from the east. GFS fields showing the Galvez Davison Index (GDI) that is sometimes used to anticipate rain in [&hellip;]<\/p>\n","protected":false},"author":19,"featured_media":61176,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[114,16,79,93],"tags":[],"class_list":["post-61175","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-18","category-heavy-rain-flooding","category-microwave","category-mirs"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/61175","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=61175"}],"version-history":[{"count":8,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/61175\/revisions"}],"predecessor-version":[{"id":61209,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/61175\/revisions\/61209"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/61176"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=61175"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=61175"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=61175"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}