{"id":6519,"date":"2024-05-31T09:48:02","date_gmt":"2024-05-31T14:48:02","guid":{"rendered":"https:\/\/inside.nssl.noaa.gov\/nsslnews\/?p=6519"},"modified":"2024-06-13T13:35:55","modified_gmt":"2024-06-13T18:35:55","slug":"lift-project-intercepts-violent-tornado-collects-historic-data","status":"publish","type":"post","link":"https:\/\/inside.nssl.noaa.gov\/nsslnews\/2024\/05\/lift-project-intercepts-violent-tornado-collects-historic-data\/","title":{"rendered":"SCIENCE IMPACT: &#8220;LIFT&#8221; project intercepts violent tornado; collects historic data"},"content":{"rendered":"\n<hr class=\"wp-block-separator has-alpha-channel-opacity\" \/>\n\n\n\n<p>Last week, NSSL\u2019s Low-Level Internal Flows in Tornadoes experiment, or \u201cLIFT\u201d, intercepted a violent tornado southeast of Duke, Okla., gathering a data set that could prove to be significant in our understanding of tornado winds at the ground level.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><a href=\"https:\/\/inside.nssl.noaa.gov\/nsslnews\/wp-content\/uploads\/sites\/21\/2024\/05\/Duke-OK-tornado.gif1_.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"600\" height=\"338\" src=\"https:\/\/inside.nssl.noaa.gov\/nsslnews\/wp-content\/uploads\/sites\/21\/2024\/05\/Duke-OK-tornado.gif1_.gif\" alt=\"\" class=\"wp-image-6544\" \/><\/a><figcaption class=\"wp-element-caption\">A violent tornado impacts the Duke, Okla., area on May 25, 2024. Researchers with NSSL&#8217;s &#8220;LIFT&#8221; project intercepted the storm and collected a historic data set very near this tornado.<\/figcaption><\/figure>\n\n\n\n<p>Researchers with LIFT seek to gather data to characterize tornado flows in the level of the atmosphere where they impact humans; the lowest 50-100 feet of the atmosphere. This area of tornadoes is still relatively unknown compared to upper air areas.&nbsp;<\/p>\n\n\n\n<p>To accomplish this objective, LIFT scientists scan tornadoes from very close range (within a mile or two) with <a href=\"https:\/\/www.nssl.noaa.gov\/tools\/radar\/mobile\/\">mobile radars<\/a>, Doppler lidar, and other NSSL-innovated platforms.&nbsp;<\/p>\n\n\n\n<p>In the<a href=\"https:\/\/forecast.weather.gov\/product.php?site=NWS&amp;issuedby=OUN&amp;product=PNS\"> Duke OK event<\/a>, a <a href=\"https:\/\/www.depts.ttu.edu\/nwi\/research\/facilities\/ka-band-radar.php\">Texas Tech University mobile Doppler radar<\/a> obtained data from less than one mile from the violent tornado. This high-resolution radar scanned the near-ground portion of the tornado.<\/p>\n\n\n\n<figure class=\"wp-block-video aligncenter\"><video height=\"1080\" style=\"aspect-ratio: 1920 \/ 1080;\" width=\"1920\" controls src=\"https:\/\/inside.nssl.noaa.gov\/nsslnews\/wp-content\/uploads\/sites\/21\/2024\/05\/20240523_PPIs_noWM.mp4\"><\/video><figcaption class=\"wp-element-caption\">Radar reflectivity and velocity captured by a <a href=\"https:\/\/www.depts.ttu.edu\/nwi\/research\/facilities\/ka-band-radar.php\">Texas Tech University mobile Doppler radar<\/a> from less than one mile from the violent Duke, Okla., tornado. This high-resolution radar scan is from the near-ground portion of the tornado.<\/figcaption><\/figure>\n\n\n\n<p>Additionally, with other research groups in the area, there were at least five mobile Dopplers capturing data on this tornado at various close ranges. Post-storm damage analysis from <a href=\"https:\/\/inside.nssl.noaa.gov\/uas\/\">uncrewed aerial systems (UAS)<\/a>, another component of the LIFT project, as well as high-resolution satellite imagery, will further help researchers characterize the nature of the tornado winds at the ground. Extensive photographic data will also augment the analysis.<br><br>The Duke tornado was LIFT\u2019s second intercept in just one week, and with such a robust data set is likely to end up as one of the most-studied tornadoes ever after the research is complete.<\/p>\n\n\n\n<p>LIFT is supported by <a href=\"https:\/\/www.nssl.noaa.gov\/projects\/vortexse\/\">VORTEX<\/a> and is a collaboration of NSSL, Texas Tech University and the Cooperative Institute for Severe and High-Impact Weather Research and Operations(CIWRO).<\/p>\n\n\n\n<div class=\"wp-block-essential-blocks-image-gallery  root-eb-image-gallery-1q49r\"><div class=\"eb-parent-wrapper eb-parent-eb-image-gallery-1q49r \"><div class=\"eb-gallery-img-wrapper eb-image-gallery-1q49r masonry overlay-bottom caption-style-0   no-isotope \" data-id=\"eb-image-gallery-1q49r\"><a href=\"https:\/\/inside.nssl.noaa.gov\/nsslnews\/wp-content\/uploads\/sites\/21\/2024\/05\/IMG_0224-3.png\" rel=\"noopener\" data-fslightbox=\"gallery\" data-type=\"image\" class=\"eb-gallery-img-content eb-filter-img-\"><span class=\"eb-gallery-link-wrapper\"><img decoding=\"async\" class=\"eb-gallery-img\" src=\"https:\/\/inside.nssl.noaa.gov\/nsslnews\/wp-content\/uploads\/sites\/21\/2024\/05\/IMG_0224-3.png\" alt=\"\" \/><\/span><\/a><a href=\"https:\/\/inside.nssl.noaa.gov\/nsslnews\/wp-content\/uploads\/sites\/21\/2024\/05\/IMG_0619-scaled.jpg\" rel=\"noopener\" data-fslightbox=\"gallery\" data-type=\"image\" class=\"eb-gallery-img-content eb-filter-img-\"><span class=\"eb-gallery-link-wrapper\"><img decoding=\"async\" class=\"eb-gallery-img\" src=\"https:\/\/inside.nssl.noaa.gov\/nsslnews\/wp-content\/uploads\/sites\/21\/2024\/05\/IMG_0619-scaled.jpg\" alt=\"\" \/><\/span><\/a><a href=\"https:\/\/inside.nssl.noaa.gov\/nsslnews\/wp-content\/uploads\/sites\/21\/2024\/05\/IMG_0621-scaled.jpg\" rel=\"noopener\" data-fslightbox=\"gallery\" data-type=\"image\" class=\"eb-gallery-img-content eb-filter-img-\"><span class=\"eb-gallery-link-wrapper\"><img decoding=\"async\" class=\"eb-gallery-img\" src=\"https:\/\/inside.nssl.noaa.gov\/nsslnews\/wp-content\/uploads\/sites\/21\/2024\/05\/IMG_0621-scaled.jpg\" alt=\"\" \/><\/span><\/a><a href=\"https:\/\/inside.nssl.noaa.gov\/nsslnews\/wp-content\/uploads\/sites\/21\/2024\/05\/IMG_0223-2-scaled.jpg\" rel=\"noopener\" data-fslightbox=\"gallery\" data-type=\"image\" class=\"eb-gallery-img-content eb-filter-img-\"><span class=\"eb-gallery-link-wrapper\"><img decoding=\"async\" class=\"eb-gallery-img\" src=\"https:\/\/inside.nssl.noaa.gov\/nsslnews\/wp-content\/uploads\/sites\/21\/2024\/05\/IMG_0223-2-scaled.jpg\" alt=\"\" \/><\/span><\/a><a href=\"https:\/\/inside.nssl.noaa.gov\/nsslnews\/wp-content\/uploads\/sites\/21\/2024\/05\/IMG_0607-1-scaled.jpg\" rel=\"noopener\" data-fslightbox=\"gallery\" data-type=\"image\" class=\"eb-gallery-img-content eb-filter-img-\"><span class=\"eb-gallery-link-wrapper\"><img decoding=\"async\" class=\"eb-gallery-img\" src=\"https:\/\/inside.nssl.noaa.gov\/nsslnews\/wp-content\/uploads\/sites\/21\/2024\/05\/IMG_0607-1-scaled.jpg\" alt=\"\" \/><\/span><\/a><\/div><\/div><\/div>\n","protected":false},"excerpt":{"rendered":"<p>NSSL\u2019s Low-Level Internal Flows in Tornadoes experiment, or \u201cLIFT\u201d, intercepted a violent tornado southeast of Duke, Okla., gathering a data set that could prove to be significant in our understanding of tornado winds at the ground level.<\/p>\n","protected":false},"author":186,"featured_media":6550,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"_eb_attr":"","ghostkit_customizer_options":"","ghostkit_custom_css":"","ghostkit_custom_js_head":"","ghostkit_custom_js_foot":"","ghostkit_typography":"","footnotes":""},"categories":[1,12,631],"tags":[622,476],"class_list":["post-6519","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-news","category-research-news","category-tornado","tag-featured","tag-tornado"],"acf":[],"wps_subtitle":"","_links":{"self":[{"href":"https:\/\/inside.nssl.noaa.gov\/nsslnews\/wp-json\/wp\/v2\/posts\/6519","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/inside.nssl.noaa.gov\/nsslnews\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/inside.nssl.noaa.gov\/nsslnews\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/nsslnews\/wp-json\/wp\/v2\/users\/186"}],"replies":[{"embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/nsslnews\/wp-json\/wp\/v2\/comments?post=6519"}],"version-history":[{"count":14,"href":"https:\/\/inside.nssl.noaa.gov\/nsslnews\/wp-json\/wp\/v2\/posts\/6519\/revisions"}],"predecessor-version":[{"id":6561,"href":"https:\/\/inside.nssl.noaa.gov\/nsslnews\/wp-json\/wp\/v2\/posts\/6519\/revisions\/6561"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/nsslnews\/wp-json\/wp\/v2\/media\/6550"}],"wp:attachment":[{"href":"https:\/\/inside.nssl.noaa.gov\/nsslnews\/wp-json\/wp\/v2\/media?parent=6519"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/nsslnews\/wp-json\/wp\/v2\/categories?post=6519"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/nsslnews\/wp-json\/wp\/v2\/tags?post=6519"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}