{"id":54531,"date":"2023-09-19T12:59:59","date_gmt":"2023-09-19T12:59:59","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=54531"},"modified":"2023-09-22T16:48:30","modified_gmt":"2023-09-22T16:48:30","slug":"haze-propagating-across-the-pacific-ocean","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/54531","title":{"rendered":"Haze propagating across the Pacific Ocean"},"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\/09\/CSPPGeo_12-19Sept2023_0400stepanim.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"1280\" height=\"720\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/09\/CSPPGeo_12-19Sept2023_0400stepanim.gif\" alt=\"\" class=\"wp-image-54532\"\/><\/a><\/figure>\n\n\n\n<p class=\"wp-block-paragraph\">Daily imagery from the <a href=\"https:\/\/geosphere.ssec.wisc.edu\/#coordinate:0,0;\">CSPP Geosphere<\/a> website above, at <a href=\"https:\/\/geosphere.ssec.wisc.edu\/#coordinate:-1947732,1925621;zoom:2.5;satellite:goeswest;num_frames:8;frame_stride:144;start_time:2023-09-12T04:00:00Z;timeframe:Start%20Time;\">0400 UTC from 12-19 September<\/a>, show  haze (highlighted by the blue arrows) moving across the Pacific Ocean.  The haze is likely a by-product of the ongoing eruption at <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/54394\">Kilauea<\/a>.  The initial burst of haze moved beyond the view of GOES-West by 19 September, but imagery shows other regions of haze are following behind.  The haze has moved into the western Pacific, and has affected visibility in the northern Marianas Islands, as noted in the <a href=\"https:\/\/forecast.weather.gov\/product.php?site=GUM&amp;issuedby=GUM&amp;product=AFD&amp;format=CI&amp;version=1&amp;glossary=1\">Forecast Discussion<\/a> from the <a href=\"https:\/\/weather.gov\/gum\">National Weather Service in Guam<\/a>, shown below.<\/p>\n\n\n\n<pre class=\"wp-block-code\"><code>Multi-spectral satellite imagery from earlier this morning showed a\nnarrow band of haze reaching the Marianas along easterly trade-wind\nflow pointing back to the Hawaii region. This haze has occasionally\ndropped visibility at the Saipan airport earlier this morning, but\nappears to have improved slightly in the afternoon hours. It is\nlikely that this haze originated from the recent Kilauea activity\nfrom September 10th-16th of last week. High uncertainty remains to\nexactly for how long this haze might persist, but it is expected to\nbe perceivable through at least Wednesday morning.<\/code><\/pre>\n\n\n\n<p class=\"wp-block-paragraph\">The image below, from the <a href=\"https:\/\/www.facebook.com\/NWSGuam\">Guam NWS Facebook page<\/a>, shows <a href=\"https:\/\/www.facebook.com\/NWSGuam\/posts\/pfbid0roimcVLjS31akWRZSKUgQz7Qi6D8inyRpdYVA4JGUGf6CHQ1qbbB7qqp3cSvwr68l\">Garapan on Saipan<\/a>.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"862\" height=\"647\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/09\/GarapanSaipan_19Sept2023.png\" alt=\"\" class=\"wp-image-54536\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/09\/GarapanSaipan_19Sept2023.png 862w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/09\/GarapanSaipan_19Sept2023-300x225.png 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/09\/GarapanSaipan_19Sept2023-768x576.png 768w\" sizes=\"auto, (max-width: 862px) 100vw, 862px\" \/><\/figure>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<p class=\"wp-block-paragraph\">The progression of haze from Hawaii to the Marianas is more easily viewed in a map that includes both Hawaii and Guam.  Daily views (all at 0400 UTC as in the animation above) of GOES-18 Band 1 (0.47 \u00b5m) imagery show the haze approaching the Marianas by 0400 UTC on 18 September.<\/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\/09\/G18Band01-20230913-0918_0400stepanim.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"1295\" height=\"425\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/09\/G18Band01-20230913-0918_0400stepanim.gif\" alt=\"\" class=\"wp-image-54539\"\/><\/a><figcaption class=\"wp-element-caption\">GOES-18 Band 1 (0.47 \u00b5m) imagery, 0400 UTC on 13 through 18 September 2023 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p class=\"wp-block-paragraph\">The toggle below of GOES-18 and Himawari-9 Band 1 imagery, both at 0400 UTC on 17 September, shows the importance of view angle relative to the Sun in detecting the presence of haze.  Haze that is apparent in GOES-18 imagery (near 160<sup>o<\/sup>E) is not apparent in Himawari-9 imagery because of differences in view angle and the location of the Sun relative to the satellite.<\/p>\n\n\n\n<figure class=\"wp-block-image size-large is-resized\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/09\/G18H9Band01-20230917_0400toggle.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/09\/G18H9Band01-20230917_0400toggle.gif\" alt=\"\" class=\"wp-image-54542\" style=\"width:1086px;height:356px\" width=\"1086\" height=\"356\"\/><\/a><figcaption class=\"wp-element-caption\">GOES_18 and Himawari-9 &#8220;Blue Visible&#8221; (Band 1, 0.47) imagery, 0400 UTC on 17 September 2023 (Click to enlarge)<\/figcaption><\/figure>\n\n\n<p style=\"text-align: center;\">_________________________________________<\/p>\n<div style=\"width: 2110px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/09\/230913_230918_himawari9_trueColorRGB_Kilauea_haze_transport_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/09\/Himawari-9_AHI_FLDK_true_color_2023259_210000Z.png\" width=\"2100\" height=\"700\" \/><\/a><p class=\"wp-caption-text\">JMA Himawari-9 True Color RGB images from 2000-2350 UTC on 13-18 September (courtesy Scott Bachmeier, CIMSS) [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/09\/230913_230918_himawari9_trueColorRGB_Kilauea_haze_transport_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n<p><a href=\"https:\/\/www.jma.go.jp\/jma\/indexe.html\"><strong>JMA<\/strong><\/a>\u00a0Himawari-9 True Color RGB images created using\u00a0<a href=\"https:\/\/www.ssec.wisc.edu\/software\/geo2grid\/\"><strong>Geo2Grid<\/strong><\/a>\u00a0<em><strong>(above)<\/strong><\/em> helped to highlight the westward transport of hazy <a href=\"https:\/\/www.usgs.gov\/observatories\/hawaiian-volcano-observatory\/frequently-asked-questions-about-volcanic-smog-vog\"><strong>volcanic smog<\/strong><\/a> (vog) from Hawai`i to the Mariana Islands during the 13-18 September time period. A plot of surface report data from Saipan Island <em><strong>(below)<\/strong><\/em> indicated that the surface visibility dropped as low as 5-6 miles (from 2100-2200 UTC on 18 September, or 7-8 AM ChST on 19 September) when the vog arrived. The satellite imagery was certainly convincing, but <a href=\"https:\/\/www.arl.noaa.gov\/hysplit\/\"><strong>HYSPLIT<\/strong><\/a> model <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/09\/230918_1800utc_10_250_500m_PGSN_trajectories.gif\"><strong>back trajectories<\/strong><\/a> also helped to implicate Kilauea vog as the source of haziness observed at Saipan (with subsidence occurring during the period of long-range transport).<\/p>\n<div style=\"width: 1290px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/09\/230918_230919_PGSN_SFCMG.GIF\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/09\/230918_230919_PGSN_SFCMG.GIF\" width=\"1280\" height=\"960\" \/><\/a><p class=\"wp-caption-text\">Plot of surface report data from Saipan Island (courtesy Scott Bachmeier, CIMSS) [click to enlarge]<\/p><\/div>\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<p class=\"wp-block-paragraph\">Thanks to Brandon Aydlett, the Science and Operations Officer at Guam, for the alert on the haze.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Daily imagery from the CSPP Geosphere website above, at 0400 UTC from 12-19 September, show haze (highlighted by the blue arrows) moving across the Pacific Ocean. The haze is likely a by-product of the ongoing eruption at Kilauea. The initial burst of haze moved beyond the view of GOES-West by 19 September, but imagery shows [&hellip;]<\/p>\n","protected":false},"author":19,"featured_media":54535,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[7,114,73,45],"tags":[],"class_list":["post-54531","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-air-quality","category-goes-18","category-himawari-9","category-redgreenblue-rgb-images"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/54531","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=54531"}],"version-history":[{"count":15,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/54531\/revisions"}],"predecessor-version":[{"id":54617,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/54531\/revisions\/54617"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/54535"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=54531"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=54531"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=54531"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}