{"id":31077,"date":"2018-12-15T23:59:57","date_gmt":"2018-12-15T23:59:57","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=31077"},"modified":"2018-12-17T18:53:29","modified_gmt":"2018-12-17T18:53:29","slug":"southern-us-storm-and-a-tehuano-wind-event","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/31077","title":{"rendered":"Southern US storm, and a Tehuano wind event"},"content":{"rendered":"<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/181213_181215_goes16_waterVapor_Southern_US_anim.mp4\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/G16_WV_SOUTHERN_US_STORM_13_15DEC2018_2018348_150217_GOES-16_0001PANEL.GIF\" alt=\"GOES-16 Low-level Water Vapor (7.3 \u00b5m) images, 13-15 December [click to play MP4 animation]\" width=\"640\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">GOES-16 Low-level Water Vapor <em>(7.3 \u00b5m)<\/em> images, 13-15 December [click to play MP4 animation]<\/p><\/div>A large midlatitude cyclone moved from the southern High Plains to the Lower Mississippi Valley during the <a href=\"https:\/\/www.wpc.ncep.noaa.gov\/dailywxmap\/index_20181213.html\"><strong>13 December<\/strong><\/a> &#8211; <a href=\"https:\/\/www.wpc.ncep.noaa.gov\/dailywxmap\/index_20181215.html\"><strong>15 December 2018<\/strong><\/a> period (<strong><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/181213_181215_surface_analyses_Southern_US_anim.gif\">surface analyses<\/a><\/strong>) &#8212; GOES-16 <em>(GOES-East)<\/em> Low-level Water Vapor (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band10.pdf\"><strong>7.3 \u00b5m<\/strong><\/a>) images <em><strong>(above)<\/strong><\/em> showed the evolution of this system.<\/p>\n<p>The corresponding GOES-16 Water Vapor images with plots of hourly surface wind gusts are shown below; <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/181213_181214_peak_winds.text\"><strong>peak wind gusts<\/strong><\/a> exceeding 50 knots occurred in parts of Colorado, New Mexico and Texas on 13 December.<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/181213_181215_goes16_waterVapor_windGusts_Southern_US_anim.mp4\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/G16_WV_GUSTS_SOUTHERN_US_STORM_13_15DEC2018_2018348_150217_GOES-16_0001PANEL.GIF\" alt=\"GOES-16 Low-level Water Vapor (7.3 \u00b5m) images with hourly plots of surface wind gusts, 13-15 December [click to play MP4 animation]\" width=\"640\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">GOES-16 Low-level Water Vapor <em>(7.3 \u00b5m)<\/em> images with hourly plots of surface wind gusts in knots, 13-15 December [click to play MP4 animation]<\/p><\/div>This event was unusually windy in South Texas and the Rio Grande Valley:<br \/>\n<center><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p dir=\"ltr\" lang=\"en\">Fun fact: Our office has only issued 4 &#8216;High Wind Warnings&#8217; over the past 30 years, including today&#8217;s. Our last &#8216;High Wind Warning&#8217; was issued February 25, 2013 for Zapata, Jim Hogg, Starr, and Brooks Counties. <a href=\"https:\/\/twitter.com\/hashtag\/funfact?src=hash&amp;ref_src=twsrc%5Etfw\">#funfact<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/txwx?src=hash&amp;ref_src=twsrc%5Etfw\">#txwx<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/NWSBrownsville?src=hash&amp;ref_src=twsrc%5Etfw\">#NWSBrownsville<\/a><\/p>\n<p>\u2014 NWS Brownsville (@NWSBrownsville) <a href=\"https:\/\/twitter.com\/NWSBrownsville\/status\/1073238892562788352?ref_src=twsrc%5Etfw\">December 13, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/center><\/p>\n<p>Another notable aspect of this storm was a very localized area of heavy snowfall just south of Sweetwater, Texas:<br \/>\n<center><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p dir=\"ltr\" lang=\"en\">Here are the observed snow totals from Thursday afternoon through Friday morning. Highest snow amounts occurred in <a href=\"https:\/\/twitter.com\/hashtag\/NolanCounty?src=hash&amp;ref_src=twsrc%5Etfw\">#NolanCounty<\/a>, where generally 3-8 inches fell. <a href=\"https:\/\/twitter.com\/hashtag\/Blackwell?src=hash&amp;ref_src=twsrc%5Etfw\">#Blackwell<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/txwx?src=hash&amp;ref_src=twsrc%5Etfw\">#txwx<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/sjtwx?src=hash&amp;ref_src=twsrc%5Etfw\">#sjtwx<\/a> <a href=\"https:\/\/t.co\/2EBzbtCgnz\">pic.twitter.com\/2EBzbtCgnz<\/a><\/p>\n<p>\u2014 NWS San Angelo (@NWSSanAngelo) <a href=\"https:\/\/twitter.com\/NWSSanAngelo\/status\/1073612024532398080?ref_src=twsrc%5Etfw\">December 14, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/center><br \/>\nThe remnant patch of snow cover was evident in VIIRS Visible (0.64 \u00b5m) and Near-Infrared &#8220;Snow\/Ice&#8221; (1.61 \u00b5m) imagery on 14 and 15 December <em><strong>(below)<\/strong><\/em>. The heaviest snowfall occurred over an isolated ridge along the eastern edge of the Edwards Plateau, where elevations of 2500-2600 feet were about 500 feet higher than the adjacent rolling plains. Since snow is a very effective absorber of energy at the 1.61 \u00b5m wavelength, it appeared <em>dark<\/em> on the Snow\/Ice imagery.<\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/181214_1917utc_suomiNPP_viirs_visible_snowIce_topography_TX_snowcover_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/181214_1917utc_suomiNPP_viirs_visible_snowIce_topography_TX_snowcover_anim.gif\" alt=\"Topography, Suomi NPP VIIRS Visible (0.64 \u00b5m) and Near-Infrared &quot;Snow\/Ice&quot; (1.61 \u00b5m) images on 14 December [click to enlarge]\" width=\"641\" height=\"370\" \/><\/a><p class=\"wp-caption-text\">Topography plus Suomi NPP VIIRS Visible <em>(0.64 \u00b5m)<\/em> and Near-Infrared &#8220;Snow\/Ice&#8221; <em>(1.61 \u00b5m)<\/em> images on 14 December [click to enlarge]<\/p><\/div><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/181215_1858utc_noaa20_viirs_visible_snowIce_topography_TX_snowcover_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/181215_1858utc_noaa20_viirs_visible_snowIce_topography_TX_snowcover_anim.gif\" alt=\"Topography plus NOAA-20 VIIRS Visible (0.64 \u00b5m) and Near-Infrared &quot;Snow\/Ice&quot; (1.61 \u00b5m) images on 15 December [click to enlarge]\" width=\"641\" height=\"370\" \/><\/a><p class=\"wp-caption-text\">Topography plus NOAA-20 VIIRS Visible <em>(0.64 \u00b5m)<\/em> and Near-Infrared &#8220;Snow\/Ice&#8221; <em>(1.61 \u00b5m)<\/em> images on 15 December [click to enlarge]<\/p><\/div>The residual snow cover on 14 December was also seen in Terra\/Aqua MODIS True Color and False Color Red-Green-Blue (RGB) images, viewed using <a href=\"http:\/\/realearth.ssec.wisc.edu\"><strong>RealEarth<\/strong><\/a> <em><strong>(below)<\/strong><\/em>. The snow appeared as shades of cyan in the False Color images.<\/p>\n<p><div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/181214_terra_aqua_modis_truecolor_falsecolor_TX_snowcover_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/181214_terra_aqua_modis_truecolor_falsecolor_TX_snowcover_anim.gif\" alt=\"Terra\/Aqua MODIS True Color and False Color images on 14 December [click to enlarge]\" width=\"642\" height=\"357\" \/><\/a><p class=\"wp-caption-text\">Terra\/Aqua MODIS True Color and False Color images on 14 December [click to enlarge]<\/p><\/div>A toggle between Terra MODIS True Color RGB images on the late morning of 14 and 15 December <em><strong>(below)<\/strong> <\/em>demonstrated the amount of snow melt in 24 hours.<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/181214_181215_terra_modis_truecolor_TX_snowcover_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/181214_181215_terra_modis_truecolor_TX_snowcover_anim.gif\" alt=\"Terra MODIS True Color RGB images on 14 and 15 December [click to enlarge]\" width=\"640\" height=\"356\" \/><\/a><p class=\"wp-caption-text\">Terra MODIS True Color RGB images on 14 and 15 December [click to enlarge]<\/p><\/div>The strong cold front associated with this storm moved rapidly southward across the western Gulf of Mexico on 14 December (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/181214_181215_surface_analyses_Gulf_of_Mexico_anim.gif\"><strong>surface analyses<\/strong><\/a>), crossing the <strong><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/Mexico_topo_2.png\">terrain of the Isthmus of Tehuantepec<\/a><\/strong> in southern Mexico and emerging into the Gulf of Tehuantepec as a gap wind (known as a <a href=\"https:\/\/en.wikipedia.org\/wiki\/Tehuantepecer\"><strong>Tehuano wind<\/strong><\/a>). A curved rope cloud marking the leading edge of the Tehuano winds was evident on GOES-17 and GOES-16 &#8220;Red&#8221; Visible (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band02.pdf\"><strong>0.64 \u00b5m<\/strong><\/a>) images <em><strong>(below)<\/strong><\/em>.<\/p>\n<p style=\"text-align: center;\"><em>* GOES-17 images shown here are preliminary and non-operational *<\/em><\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/181214_goes17_goes17_visible_Tehuano_Wind_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/G17_G16_VIS_TEHUANO_14DEC2018_2018348_213038_GOES-16_0002PANELS.GIF\" alt=\"GOES-17 (left) and GOES-16 (right) \" width=\"640\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">GOES-17 <em>(left)<\/em> and GOES-16 <em>(right)<\/em> &#8220;Red&#8221; Visible <em>(0.64 \u00b5m)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/181214_goes17_goes17_visible_Tehuano_Wind_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>A comparison of GOES-16 Visible imagery from 14 and 15 December<em><strong> (below)<\/strong><\/em> showed how far southwestward the gap winds spread out across the Pacific Ocean during those 2 days. Note that on 15 December there were ship reports with wind speeds of 50 knots, at <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/G16_VIS_TEHUANO_15DEC2018_2018349_124534_GOES-16_0001PANEL.GIF\"><strong>12 UTC<\/strong><\/a> and at <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/G16_VIS_TEHUANO_15DEC2018_2018349_170034_GOES-16_0001PANEL.GIF\"><strong>17 UTC<\/strong><\/a>.<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/181214_181215_goes16_visible_Tehuano_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/G16_VIS_TEHUANO_15DEC2018_2018349_190034_GOES-16_0001PANEL.GIF\" alt=\"GOES-16 \" width=\"640\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">GOES-16 &#8220;Red&#8221; Visible <em>(0.64 \u00b5m)<\/em> images with surface and ship reports, 14-15 December [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/181214_181215_goes16_visible_Tehuano_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>NOAA-20 VIIRS True Color RGB and Infrared Window (11.45 \u00b5m) images on 14 and 15 December <em><strong>(below)<\/strong><\/em> also showed the progression of the Tehuano wind rope cloud &#8212; the hazy signature of dust-laden air within the offshore flow was also apparent on the daytime True Color images.<\/p>\n<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/181214_181215_noaa20_viirs_truecolor_infrared_Tehuano_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/181214_181215_noaa20_viirs_truecolor_infrared_Tehuano_anim.gif\" alt=\"NOAA-20 VIIRS True Color and Infrared Window (11.45 \u00b5m) images on 14 and 15 December [click to enlarge]\" width=\"640\" height=\"357\" \/><\/a><p class=\"wp-caption-text\">NOAA-20 VIIRS True Color RGB and Infrared Window <em>(11.45 \u00b5m)<\/em> images on 14 and 15 December [click to enlarge]<\/p><\/div>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/181214_metop_ascat_Gulf_of_Mexico_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/181214_metop_ascat_Gulf_of_Mexico_anim.gif\" alt=\"Metop-A and Metop-B ASCAT surface scatterometer winds across the western Gulf of Mexico [click to enlarge]\" width=\"640\" height=\"564\" \/><\/a><p class=\"wp-caption-text\">Metop-A and Metop-B ASCAT surface scatterometer winds across the western Gulf of Mexico [click to enlarge]<\/p><\/div>On 14 December, a sequence of <a href=\"https:\/\/www.eumetsat.int\/website\/home\/index.html\"><strong>EUMETSAT<\/strong><\/a> Metop-A and Metop-B <a href=\"https:\/\/www.eumetsat.int\/website\/home\/Satellites\/CurrentSatellites\/Metop\/MetopDesign\/ASCAT\/index.html\"><strong>ASCAT<\/strong><\/a> surface scatterometer winds (<a href=\"https:\/\/manati.star.nesdis.noaa.gov\/datasets\/ASCATData.php\"><strong>source<\/strong><\/a>) showed the cold front moving southward across the western Gulf of Mexico <em><strong>(above)<\/strong>,<\/em> and also showed the northerly gap wind flow just beginning to emerge into the Gulf of Tehuantepec around 1607 UTC <em><strong>(below)<\/strong><\/em>.<\/p>\n<p><div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/181214_metop_ascat_Tehuano_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/181214_metop_ascat_Tehuano_anim.gif\" alt=\"Metop-A and Metop-B ASCAT surface scatterometer winds across the southern Gulf of Mexico and the Gulf of Tehuantepec [click to enlarge]\" width=\"642\" height=\"563\" \/><\/a><p class=\"wp-caption-text\">Metop-A and Metop-B ASCAT surface scatterometer winds across the far southern Gulf of Mexico and the Gulf of Tehuantepec [click to enlarge]<\/p><\/div>The plume of dry air being transported southwestward across the Pacific Ocean by the gap winds was apparent on <a href=\"http:\/\/tropic.ssec.wisc.edu\/real-time\/mtpw2m\/product.php?color_type=tpw_nrl_colors&amp;layer=700-850&amp;prod=conus&amp;timespan=48hrs&amp;anim=html5\"><strong>MIMIC Total Precipitable Water<\/strong><\/a> images <em><strong>(below)<\/strong><\/em>. The majority of this dry air was within the surface-850 hPa layer (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/181215_21utc_mimicTPW_anim.gif\"><strong>21 UTC comparison<\/strong><\/a>).<\/p>\n<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/181214_181215_mtpw_sfc850_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/12\/181215_21z_mtpw_tpw.png\" alt=\"MIMIC Total Precipitable Water product (Total column, and Surface-850 hPa layer) [click to play animation]\" width=\"640\" height=\"300\" \/><\/a><p class=\"wp-caption-text\">MIMIC Total Precipitable Water product (Total column, and Surface-850 hPa layer) [click to play animation]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>A large midlatitude cyclone moved from the southern High Plains to the Lower Mississippi Valley during the 13 December &#8211; 15 December 2018 period (surface analyses) &#8212; GOES-16 (GOES-East) Low-level Water Vapor (7.3 \u00b5m) images (above) showed the evolution of this system. The corresponding GOES-16 Water Vapor images with plots of hourly surface wind gusts [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":31087,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[70,74,80,58,12,78,53,45,25,49,71,48],"tags":[],"class_list":["post-31077","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-aqua","category-goes-16","category-goes-17","category-metop","category-modis","category-noaa-20","category-real-earth","category-redgreenblue-rgb-images","category-satellite-winds","category-suomi_npp","category-terra","category-viirs"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/31077","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=31077"}],"version-history":[{"count":22,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/31077\/revisions"}],"predecessor-version":[{"id":31101,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/31077\/revisions\/31101"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/31087"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=31077"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=31077"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=31077"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}