{"id":51808,"date":"2023-04-20T20:14:05","date_gmt":"2023-04-20T20:14:05","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=51808"},"modified":"2023-04-20T20:27:50","modified_gmt":"2023-04-20T20:27:50","slug":"probsevere-in-the-oklahoma-severe-weather-outbreak","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/51808","title":{"rendered":"ProbSevere in the Oklahoma severe-weather outbreak"},"content":{"rendered":"\n<p>There was a conditional outlook for severe storms in Oklahoma on April 19th, owing to uncertainty in the forcing for ascent and a stout warm-sector cap. Well, the cap broke, and mayhem ensued in central Oklahoma. <br><br>A break in the cirrus deck in southwest Oklahoma likely contributed to surface heating and enhanced mixing of the boundary layer, allowing the cap to break. <a href=\"https:\/\/cimss.ssec.wisc.edu\/severe_conv\/pltg.html\">ProbSevere LightningCast<\/a>, an AI model that uses solely images of ABI data to predict next-hour lightning at any given point, was able to capture lightning initiation (Figure 1). Glaciating cloud tops are a prime signal of imminent lightning, and the one-minute scans from the GOES-16 mesoscale sector helped the model maximize lead time (Figure 2).<\/p>\n\n\n\n<figure class=\"wp-block-video\"><video height=\"932\" style=\"aspect-ratio: 1020 \/ 932;\" width=\"1020\" controls loop src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/04\/OK_lc_20230419.mp4\"><\/video><figcaption class=\"wp-element-caption\">Figure 1: ProbSevere LightningCast contours, GOES-16 ABI day-cloud-land RGB, and GOES-16 GLM flash-extent density.<\/figcaption><\/figure>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-large is-resized\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/04\/Screen-Shot-2023-04-20-at-2.30.16-PM-1024x927.png\" alt=\"\" class=\"wp-image-51828\" width=\"768\" height=\"695\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/04\/Screen-Shot-2023-04-20-at-2.30.16-PM-1024x927.png 1024w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/04\/Screen-Shot-2023-04-20-at-2.30.16-PM-300x272.png 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/04\/Screen-Shot-2023-04-20-at-2.30.16-PM-768x695.png 768w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/04\/Screen-Shot-2023-04-20-at-2.30.16-PM.png 1474w\" sizes=\"auto, (max-width: 768px) 100vw, 768px\" \/><figcaption class=\"wp-element-caption\">Figure 2: Electrified storms with annotations of lead time to lightning initiation or forecasts produced by LightningCast<\/figcaption><\/figure>\n<\/div>\n\n\n<p><a href=\"https:\/\/cimss.ssec.wisc.edu\/severe_conv\/psv3.html\">ProbSevere version 3<\/a>, a set of machine-learning models that predicts probabilities of severe weather hazards in the near future, was able to track these storms as they became severe (Figure 3). These storms produced huge hail (up to 3&#8243; in diameter), straight-line winds exceeding 80 mph, and deadly tornadoes (Figure 4). One aspect of ProbSevere&#8217;s automated guidance that forecasters have frequently reported is that during busy situations, ProbSevere helps them quickly triage which storms or threats to prioritize and investigate further. In this outbreak, most storms had at least severe thunderstorm warnings, while several were tornado-warned. Both ProbSevere v3 and LightningCast will be evaluated by forecasters at NOAA&#8217;s Hazardous Weather Testbed this spring.<\/p>\n\n\n\n<p><\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"1731\" height=\"1317\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/04\/OK_ps_20230419.gif\" alt=\"\" class=\"wp-image-51823\" \/><figcaption class=\"wp-element-caption\">Figure 3: ProbSevere v3 storm contours (inner contour is colored by the probability of any severe; outer contour is colored by the probability of tornado), MRMS MergedReflectivity, and NWS severe weather warnings. <\/figcaption><\/figure>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"582\" height=\"408\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/04\/SPCstorms.png\" alt=\"\" class=\"wp-image-51784\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/04\/SPCstorms.png 582w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/04\/SPCstorms-300x210.png 300w\" sizes=\"auto, (max-width: 582px) 100vw, 582px\" \/><figcaption class=\"wp-element-caption\">Figure 4: Preliminary storm reports from the Storm Prediction Center. <\/figcaption><\/figure>\n<\/div>\n\n\n<p>Just a little further north in Kansas, LightningCast was able to correctly predict lightning initiation (with about 16 minutes of lead time) for the storm despite moderate overlapping cirrus clouds (Figure 5). Despite the obscuring ice clouds, LightningCast was able to discern elevated lightning potential with the aid of the visible red band (0.64-\u00b5m reflectance), snow-ice band (1.6-\u00b5m reflectance), and long-wave infrared bands (10.3-\u00b5m and 12.3-\u00b5m brightness temperatures) and the spatial patterns evident in the growing cumuliform clouds.<\/p>\n\n\n\n<figure class=\"wp-block-video\"><video height=\"746\" style=\"aspect-ratio: 1020 \/ 746;\" width=\"1020\" controls loop src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/04\/KS_lc_20230419.mp4\"><\/video><figcaption class=\"wp-element-caption\">Figure 5: ProbSevere LightningCast contours, GOES-16 ABI day-cloud-phase-distinction RGB, and GOES-16 GLM flash-extent density.<\/figcaption><\/figure>\n\n\n\n<p><\/p>\n\n\n\n<p>In fact, for this storm, the reflective bands were quite important. When they were removed from the model (a &#8220;data-denial&#8221; experiment), the probability of lightning was &lt; 10% for this convection at 21:25 UTC, whereas the full LightningCast model produced a maximum probability of about 50% at this time (Figure 6). While we have found that LightningCast performs quite well at night (when the reflective bands are uniformly zero), moderate cirrus cover at night might be an instance where users should expect less lead time to lightning initiation.   <\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"374\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/04\/Screen-Shot-2023-04-20-at-2.45.53-PM-1024x374.png\" alt=\"\" class=\"wp-image-51837\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/04\/Screen-Shot-2023-04-20-at-2.45.53-PM-1024x374.png 1024w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/04\/Screen-Shot-2023-04-20-at-2.45.53-PM-300x109.png 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/04\/Screen-Shot-2023-04-20-at-2.45.53-PM-768x280.png 768w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/04\/Screen-Shot-2023-04-20-at-2.45.53-PM-1536x560.png 1536w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/04\/Screen-Shot-2023-04-20-at-2.45.53-PM-2048x747.png 2048w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><figcaption class=\"wp-element-caption\">Figure 6: LightningCast probabilities for the full model (&#8220;control&#8221;, left) and the model without the reflective bands (right). The background image is the day-cloud-phase-distinction RGB.<\/figcaption><\/figure>\n\n\n\n<p>Notice how difficult it is to visually pick out growing convection in this scene, with only the long-wave infrared bands plotted. LightningCast can only discern what humans are able to pick out in the satellite imagery, but LightningCast does it quickly, automatically, objectively, and without ceasing, aiding forecasters in their decision making. <\/p>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-large is-resized\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/04\/Screen-Shot-2023-04-20-at-2.53.56-PM-1024x722.png\" alt=\"\" class=\"wp-image-51839\" width=\"768\" height=\"542\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/04\/Screen-Shot-2023-04-20-at-2.53.56-PM-1024x722.png 1024w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/04\/Screen-Shot-2023-04-20-at-2.53.56-PM-300x211.png 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/04\/Screen-Shot-2023-04-20-at-2.53.56-PM-768x541.png 768w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/04\/Screen-Shot-2023-04-20-at-2.53.56-PM-1536x1082.png 1536w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/04\/Screen-Shot-2023-04-20-at-2.53.56-PM.png 2038w\" sizes=\"auto, (max-width: 768px) 100vw, 768px\" \/><figcaption class=\"wp-element-caption\">Figure 7: Predictions made by the LightningCast model <em>without<\/em> the reflective bands. The background image is an &#8220;infrared cloud phase&#8221; RGB from GOES-16, used to help discern cloud phase at nighttime.<\/figcaption><\/figure>\n<\/div>","protected":false},"excerpt":{"rendered":"<p>There was a conditional outlook for severe storms in Oklahoma on April 19th, owing to uncertainty in the forcing for ascent and a stout warm-sector cap. Well, the cap broke, and mayhem ensued in central Oklahoma. A break in the cirrus deck in southwest Oklahoma likely contributed to surface heating and enhanced mixing of the [&hellip;]<\/p>\n","protected":false},"author":14,"featured_media":51828,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[115,59],"tags":[84,111,87],"class_list":["post-51808","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-lightningcast","category-probsevere","tag-goes-16","tag-lightningcast","tag-probsevere"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/51808","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\/14"}],"replies":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/comments?post=51808"}],"version-history":[{"count":12,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/51808\/revisions"}],"predecessor-version":[{"id":51846,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/51808\/revisions\/51846"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/51828"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=51808"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=51808"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=51808"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}