{"id":35406,"date":"2020-01-12T23:59:13","date_gmt":"2020-01-12T23:59:13","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=35406"},"modified":"2020-01-15T16:34:35","modified_gmt":"2020-01-15T16:34:35","slug":"eruption-of-the-taal-volcano-in-the-philippines","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/35406","title":{"rendered":"Eruption of the Taal Volcano in the Philippines"},"content":{"rendered":"<p><div style=\"width: 653px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200112_himawari8_visible_infrared_Taal_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/HIM08_VIS_IR_TAAL_12JAN2020_B313_2020012_083000_0002PANELS_FRAME00013.GIF\" alt=\"Himawari-8 \" width=\"643\" height=\"482\" \/><\/a><p class=\"wp-caption-text\">Himawari-8 &#8220;Red&#8221; Visible<em> (0.64 \u00b5m, left)<\/em> and &#8220;Clean&#8221; Infrared Window<em> (10.4 \u00b5m, right)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200112_himawari8_visible_infrared_Taal_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>The <strong><a href=\"https:\/\/en.wikipedia.org\/wiki\/Taal_Volcano\">Taal Volcano<\/a><\/strong> erupted in the Philippines around 0850 UTC on 12 January 2020. JMA Himawari-8 &#8220;Red&#8221; Visible (0.64 \u00b5m) and &#8220;Clean&#8221; Infrared Window (10.4 \u00b5m) images <em><strong>(above)<\/strong><\/em> displayed the volcanic cloud during the initial 3 hours post-eruption. Note the presence of a pronounced &#8220;warm wake&#8221;<em> (red enhancement)<\/em> downwind (north) of the summit of Taal &#8212; this appeared to be an <a href=\"https:\/\/journals.ametsoc.org\/doi\/abs\/10.1175\/WAF-D-18-0040.1?journalCode=wefo\"><strong>Above-Anvil Cirrus Plume<\/strong><\/a> (AACP), as seen in a toggle between the Visible and Infrared images at 1910 UTC<em><strong> (below)<\/strong><\/em>.<\/p>\n<p><div style=\"width: 648px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200112_0910utc_himawari8_visible_infrared_Tall_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200112_0910utc_himawari8_visible_infrared_Tall_anim.gif\" alt=\"Himawari-8 &quot;Red&quot; Visible (0.64 \u00b5m) and &quot;Clean&quot; Infrared Window (10.4 \u00b5m) images at 1910 UTC [click to enlarge]\" width=\"638\" height=\"957\" \/><\/a><p class=\"wp-caption-text\">Himawari-8 &#8220;Red&#8221; Visible <em>(0.64 \u00b5m)<\/em> and &#8220;Clean&#8221; Infrared Window<em> (10.4 \u00b5m)<\/em> images at 1910 UTC [click to enlarge]<\/p><\/div><span class=\"css-901oao css-16my406 r-1qd0xha r-ad9z0x r-bcqeeo r-qvutc0\">The warmest Himawari-8 <\/span><span class=\"css-901oao css-16my406 r-1qd0xha r-ad9z0x r-bcqeeo r-qvutc0\">10.4 \u00b5m brightness temperatures within the <\/span><span class=\"css-901oao css-16my406 r-1qd0xha r-ad9z0x r-bcqeeo r-qvutc0\">Above-Anvil Cirrus Plume were around -60\u00baC <em>(red enhancement),<\/em> which corresponded to approximately 21 km on data from 3 rawinsonde sites in the Philippines<\/span> (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200112_RPMP_RAOBS.TEXT\"><strong>Legaspi<\/strong><\/a>, <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200112_RPMT_RAOBS.TEXT\"><strong>Mactan<\/strong><\/a> and <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200112_RPLI_RAOBS.TEXT\"><strong>Laoag<\/strong><\/a>) <em><strong>(below)<\/strong><\/em>.<\/p>\n<div style=\"width: 653px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200112_RPMP_RPMT_RPLI_raobs_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200112_RPMP_RPMT_RPLI_raobs_anim.gif\" alt=\"Plots of rawinsonde data from Legaspi, Mactan and Laoag in the Philippines [click to enlarge]\" width=\"643\" height=\"482\" \/><\/a><p class=\"wp-caption-text\">Plots of rawinsonde data from Legaspi, Mactan and Laoag in the Philippines [click to enlarge]<\/p><\/div>\n<p>The <strong><a href=\"http:\/\/www.tropomi.eu\/\">TROPOMI<\/a><\/strong> detected SO2 at altitude of 20km on 13 January:<br \/>\n<center><\/p>\n<blockquote class=\"twitter-tweet\">\n<p lang=\"en\" dir=\"ltr\">The SO2 signal from <a href=\"https:\/\/twitter.com\/hashtag\/Taal?src=hash&amp;ref_src=twsrc%5Etfw\">#Taal<\/a> detected by <a href=\"https:\/\/twitter.com\/hashtag\/TROPOMI?src=hash&amp;ref_src=twsrc%5Etfw\">#TROPOMI<\/a> on 2020-01-13 has an altitude of up to 20km. <a href=\"https:\/\/twitter.com\/hashtag\/SO2LH?src=hash&amp;ref_src=twsrc%5Etfw\">#SO2LH<\/a>. <a href=\"https:\/\/twitter.com\/tropomi?ref_src=twsrc%5Etfw\">@tropomi<\/a> <a href=\"https:\/\/twitter.com\/DLR_en?ref_src=twsrc%5Etfw\">@DLR_en<\/a> <a href=\"https:\/\/twitter.com\/ESA_EO?ref_src=twsrc%5Etfw\">@ESA_EO<\/a> <a href=\"https:\/\/t.co\/x6nstNRWUw\">pic.twitter.com\/x6nstNRWUw<\/a><\/p>\n<p>&mdash; TROPOMI SO2 (@DlrSo2) <a href=\"https:\/\/twitter.com\/DlrSo2\/status\/1216701369203281920?ref_src=twsrc%5Etfw\">January 13, 2020<\/a><\/p><\/blockquote>\n<p> <script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/center><br \/>\nA longer animation of Himawari-8 Infrared imagery revealed the intermittent presence of the warm wake feature until about 1400 UTC. The coldest 10.4 \u00b5m cloud-top brightness temperature was -89.7\u00baC.<\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200112_himawari8_infrared_zoom_Taal_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/HIM08_IR_TAAL_ZOOM_12JAN2020_B13_2020012_115000_HIMAWARI-8_0001PANEL_FRAME00033.GIF\" alt=\"Himawari-8 &quot;Clean&quot; Infrared Window (10.4 \u00b5m) images [click to play animation | MP4]\" width=\"641\" height=\"641\" \/><\/a><p class=\"wp-caption-text\">Himawari-8 &#8220;Clean&#8221; Infrared Window<em> (10.4 \u00b5m)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200112_himawari8_infrared_zoom_Taal_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>A large-scale view of Himawari-8 Infrared images <em><strong>(below)<\/strong><\/em> showed that the volcanic cloud was advected a great distance north-northeastward.<\/p>\n<p><div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200112_himawari8_infrared_Taal_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/HIM08_IR_TAAL_12JAN2020_B13_2020012_115000_HIMAWARI-8_0001PANEL_FRAME00033.GIF\" alt=\"Himawari-8 &quot;Clean&quot; Infrared Window (10.4 \u00b5m) images [click to play animation | MP4]\" width=\"642\" height=\"642\" \/><\/a><p class=\"wp-caption-text\">Himawari-8 &#8220;Clean&#8221; Infrared Window <em>(10.4 \u00b5m)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200112_himawari8_infrared_Taal_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>A toggle between NOAA-20 VIIRS Day\/Night Band (0.7 \u00b5m) and Infrared Window (11.45 \u00b5m) images<em><strong> (below)<\/strong><\/em> showed the volcanic cloud at 1649 UTC.<\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200112_1648utc_noaa20_viirs_dayNightBand_infraredWindow_Taal_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200112_1648utc_noaa20_viirs_dayNightBand_infraredWindow_Taal_anim.gif\" alt=\"NOAA-20 VIIRS Day\/Night Band (0.7 \u00b5m) and Infrared Window (11.45 \u00b5m) images at 1648 UTC (credit: William Straka, CIMSS) [click to enlarge]\" width=\"641\" height=\"346\" \/><\/a><p class=\"wp-caption-text\">NOAA-20 VIIRS Day\/Night Band<em> (0.7 \u00b5m)<\/em> and Infrared Window <em>(11.45 \u00b5m)<\/em> images at 1648 UTC (credit: William Straka, CIMSS) [click to enlarge]<\/p><\/div>In a sequence of Split Window Difference (11-12 \u00b5m) images (Terra MODIS, NOAA-20 VIIRS and Suomi NPP VIIRS) from the <a href=\"http:\/\/volcano.ssec.wisc.edu\"><strong>NOAA\/CIMSS Volcanic Cloud Monitoring<\/strong><\/a> site<em><strong> (below)<\/strong>,<\/em> there was only a subtle ash signature <em>(blue enhancement)<\/em> immediately downwind of the Taal summit &#8212; due to the large amount of ice within the upper portion of the volcanic cloud, the infrared spectral ash signature was significantly masked.<\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200112_modis_viirs_splitWindowDifference_Taal_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200112_modis_viirs_splitWindowDifference_Taal_anim.gif\" alt=\"Split Window Difference (11-12 um) images from Terra MODIS, NOAA-20 VIIRS and Suomi NPP VIIRS [click to enlarge]\" width=\"641\" height=\"526\" \/><\/a><p class=\"wp-caption-text\">Split Window Difference <em>(11-12 \u00b5m)<\/em> images from Terra MODIS, NOAA-20 VIIRS and Suomi NPP VIIRS [click to enlarge]<\/p><\/div>Of interest was the fact that Manila International Airport (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200112_RPLL_OBS.TEXT\"><strong>RPLL<\/strong><\/a>) reported a thunderstorm at <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/HIM08_IR_TAAL_ZOOM_12JAN2020_B13_2020012_150000_HIMAWARI-8_0001PANEL_FRAME00051.GIF\"><strong>15 UTC<\/strong><\/a> &#8212; there was a large amount of lightning produced by Taal&#8217;s volcanic cloud.<br \/>\n<center><\/p>\n<blockquote class=\"twitter-tweet\">\n<p dir=\"ltr\" lang=\"en\"><a href=\"https:\/\/twitter.com\/hashtag\/TaalEruption?src=hash&amp;ref_src=twsrc%5Etfw\">#TaalEruption<\/a> as seen from <a href=\"https:\/\/twitter.com\/VaisalaGroup?ref_src=twsrc%5Etfw\">@VaisalaGroup<\/a> merged total lightning (NLDN and GLD) 15-min plots. This lapse is about 15 hours long and lightning activity has quieted since. ?<a href=\"https:\/\/twitter.com\/hashtag\/TaalEruption2020?src=hash&amp;ref_src=twsrc%5Etfw\">#TaalEruption2020<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/TaalVolcano?src=hash&amp;ref_src=twsrc%5Etfw\">#TaalVolcano<\/a> <a href=\"https:\/\/twitter.com\/COweatherman?ref_src=twsrc%5Etfw\">@COweatherman<\/a> <a href=\"https:\/\/t.co\/kkxjztq9KU\">pic.twitter.com\/kkxjztq9KU<\/a><\/p>\n<p>\u2014 William Churchill (@kudrios) <a href=\"https:\/\/twitter.com\/kudrios\/status\/1216586610021552130?ref_src=twsrc%5Etfw\">January 13, 2020<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\">\n<p dir=\"ltr\" lang=\"en\">Volcanic eruption at <a href=\"https:\/\/twitter.com\/hashtag\/TaalVolcano?src=hash&amp;ref_src=twsrc%5Etfw\">#TaalVolcano<\/a> with AMAZING <a href=\"https:\/\/twitter.com\/hashtag\/volcano?src=hash&amp;ref_src=twsrc%5Etfw\">#volcano<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/lightning?src=hash&amp;ref_src=twsrc%5Etfw\">#lightning<\/a> display. Remind me later to get counts. Data from <a href=\"https:\/\/twitter.com\/VaisalaGroup?ref_src=twsrc%5Etfw\">@VaisalaGroup<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/GLD360?src=hash&amp;ref_src=twsrc%5Etfw\">#GLD360<\/a>. <a href=\"https:\/\/twitter.com\/hashtag\/VaisalaDigital?src=hash&amp;ref_src=twsrc%5Etfw\">#VaisalaDigital<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/AMS2020?src=hash&amp;ref_src=twsrc%5Etfw\">#AMS2020<\/a> <a href=\"https:\/\/twitter.com\/janinekrippner?ref_src=twsrc%5Etfw\">@janinekrippner<\/a> <a href=\"https:\/\/twitter.com\/C_MarieSmith?ref_src=twsrc%5Etfw\">@C_MarieSmith<\/a> <a href=\"https:\/\/twitter.com\/volcaniclastic?ref_src=twsrc%5Etfw\">@volcaniclastic<\/a> <a href=\"https:\/\/twitter.com\/simoncarn?ref_src=twsrc%5Etfw\">@simoncarn<\/a> <a href=\"https:\/\/twitter.com\/CorCima?ref_src=twsrc%5Etfw\">@CorCima<\/a> <a href=\"https:\/\/t.co\/vYpgPJRoGC\">pic.twitter.com\/vYpgPJRoGC<\/a><\/p>\n<p>\u2014 Ch?is Vagas|?y (@COweatherman) <a href=\"https:\/\/twitter.com\/COweatherman\/status\/1216331790207635457?ref_src=twsrc%5Etfw\">January 12, 2020<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\">\n<p dir=\"ltr\" lang=\"en\">If you&#8217;re mesmerized by the steamy <a href=\"https:\/\/twitter.com\/hashtag\/Taal?src=hash&amp;ref_src=twsrc%5Etfw\">#Taal<\/a> eruption plume and wondering why it&#8217;s creating so much <a href=\"https:\/\/twitter.com\/hashtag\/VolcanicLightning?src=hash&amp;ref_src=twsrc%5Etfw\">#VolcanicLightning<\/a>, you\u2019re not alone. Here\u2019s a micro-crash course on the physics of volcanic thunderstorms for non-specialists. Thanks to <a href=\"https:\/\/twitter.com\/joshibob_?ref_src=twsrc%5Etfw\">@joshibob_<\/a> for the incredible footage! (1\/14) <a href=\"https:\/\/t.co\/CCl6zw56RZ\">pic.twitter.com\/CCl6zw56RZ<\/a><\/p>\n<p>\u2014 Alexa Van Eaton (@volcaniclastic) <a href=\"https:\/\/twitter.com\/volcaniclastic\/status\/1216579200137564160?ref_src=twsrc%5Etfw\">January 13, 2020<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/center><\/p>\n<p style=\"text-align: center;\"><strong>===== 14 January Update =====<\/strong><\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200114_goes17_so2RGB_Taal_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/g17_so2_taal-20200114_123032.png\" alt=\"GOES-17 SO2 RGB images [click to play animation | MP4]\" width=\"641\" height=\"299\" \/><\/a><p class=\"wp-caption-text\">GOES-17 SO2 RGB images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200114_goes17_so2RGB_Taal_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>2 days after the eruption, the leading edge of Taal&#8217;s SO2-rich volcanic plume <em>(brighter shades of yellow over areas of cold clouds)<\/em> began to appear within the far western view of GOES-17 <em>(GOES-West)<\/em> Full Disk <a href=\"http:\/\/rammb.cira.colostate.edu\/training\/visit\/quick_guides\/Quick_Guide_SO2_RGB.pdf\"><strong>SO2<\/strong><\/a> Red-Green-Blue (RGB) images <em><strong>(above)<\/strong>,<\/em> about 1000 miles southeast of Japan. There were also some thin filaments of SO2 <em>(brighter shades of white over warm ocean areas)<\/em> moving southward, about 1500 miles west of Hawai&#8217;i.<br \/>\n<center><\/p>\n<blockquote class=\"twitter-tweet\">\n<p lang=\"en\" dir=\"ltr\">Volcanic SO2 cloud from <a href=\"https:\/\/twitter.com\/hashtag\/TaalVolcano?src=hash&amp;ref_src=twsrc%5Etfw\">#TaalVolcano<\/a> is moving further East towards Alaska. <a href=\"https:\/\/twitter.com\/hashtag\/TROPOMI?src=hash&amp;ref_src=twsrc%5Etfw\">#TROPOMI<\/a> <a href=\"https:\/\/twitter.com\/tropomi?ref_src=twsrc%5Etfw\">@TROPOMI<\/a> <a href=\"https:\/\/twitter.com\/Sentinel5p?ref_src=twsrc%5Etfw\">@Sentinel5p<\/a> <a href=\"https:\/\/twitter.com\/ESA_EO?ref_src=twsrc%5Etfw\">@ESA_EO<\/a> <a href=\"https:\/\/twitter.com\/DLR_en?ref_src=twsrc%5Etfw\">@DLR_en<\/a> <a href=\"https:\/\/twitter.com\/BIRA_IASB?ref_src=twsrc%5Etfw\">@BIRA_IASB<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/SO2LH?src=hash&amp;ref_src=twsrc%5Etfw\">#SO2LH<\/a> <a href=\"https:\/\/t.co\/Brp4Iig0PV\">pic.twitter.com\/Brp4Iig0PV<\/a><\/p>\n<p>&mdash; TROPOMI SO2 (@DlrSo2) <a href=\"https:\/\/twitter.com\/DlrSo2\/status\/1217036606630252544?ref_src=twsrc%5Etfw\">January 14, 2020<\/a><\/p><\/blockquote>\n<p> <script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/center><\/p>\n","protected":false},"excerpt":{"rendered":"<p>The Taal Volcano erupted in the Philippines around 0850 UTC on 12 January 2020. JMA Himawari-8 &#8220;Red&#8221; Visible (0.64 \u00b5m) and &#8220;Clean&#8221; Infrared Window (10.4 \u00b5m) images (above) displayed the volcanic cloud during the initial 3 hours post-eruption. Note the presence of a pronounced &#8220;warm wake&#8221; (red enhancement) downwind (north) of the summit of Taal [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":35409,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[80,62,12,78,45,49,71,48,9],"tags":[],"class_list":["post-35406","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-17","category-himawari-8","category-modis","category-noaa-20","category-redgreenblue-rgb-images","category-suomi_npp","category-terra","category-viirs","category-volcanic-activity"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/35406","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=35406"}],"version-history":[{"count":26,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/35406\/revisions"}],"predecessor-version":[{"id":35434,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/35406\/revisions\/35434"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/35409"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=35406"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=35406"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=35406"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}