Hail, Terry
- When
- May 28, 1:25 PM CST to 1:35 PM CST
- Where
- Terry County, Wellman
- Measured
- 1 in hail
- Reported by
- Public
- Coordinates
- 33.050, -102.430
The Southwest Cotton Growers in Wellman reported quarter size hail that lasted for ten minutes.
A dryline, in combination with a westward moving outflow boundary, served as a focus for thunderstorm development on the afternoon of the 28th. Initial thunderstorm activity formed over the western South Plains and southwest Texas Panhandle where the outflow boundary met the dryline.
Every event with a place to put it; 4 filed by county or forecast zone are drawn at its center, in a lighter ring. Tap one for its entry below.
Deaths and injuries are direct and indirect together, as the offices filed them. Damage is property and crops in the dollars of the year, not adjusted for inflation, and only where an office estimated it.
The episode as NWS LUB wrote it up.
A dryline, in combination with a westward moving outflow boundary, served as a focus for thunderstorm development on the afternoon of the 28th. Initial thunderstorm activity formed over the western South Plains and southwest Texas Panhandle where the outflow boundary met the dryline. Warm temperatures into the 90s combined with good low level moisture to create a very unstable atmosphere. Strong vertical wind shear allowed thunderstorms to rotate and split creating left and right moving supercells as well as very large hail. One particularly robust supercell thunderstorm generated giant hail over the west-central South Plains. Hail as large as DVDs were observed from a storm as it tracked slowly southeastward through Hockley County. Outside of the primary thunderstorm cores, strong and severe wind gusts occurred on the backside of a decaying rain area over the south-central Texas Panhandle. These severe winds toppled some utility lines and center pivots near Plainview and Hale Center (Hale County).
A long-lived supercell thunderstorm developed near Tucumcari, New Mexico on the evening of the 28th and proceeded to move south and southeast overnight into the early morning hours of the 29th. As this storm entered western Bailey County in Texas around 2300 CST, it transitioned into a bow echo that continued to move southeast for the next four hours accompanied by destructive winds, wind-driven hail, and torrential rain. The storm finally weakened to below severe limits near Snyder around 0330 CST. The most destructive straight-line winds occurred in Levelland (Hockley County) from around 0030 CST until 0040 CST, with a second swath of intense winds impacting Tahoka (Lynn County) shortly before 0200 CST. An NWS storm survey team documented extensive wind damage primarily on the north and east sides of Levelland, with additional damage also occurring in and around Tahoka. In addition to wind damage, a few homes in Levelland had floodwaters infiltrate the structures resulting in water damage with many more suffering rainwater damage from broken windows or damaged roofs. A total of thirteen people in Levelland received minor injuries from broken glass but all were released from treatment.
High wind reports from the Texas Tech University West Texas mesonet are below:
80 mph at Olton (Lamb County),|78 mph at Aiken (Hale County),|71 mph at Hart (Castro County),|70 mph at Plainview (Hale County), and|60 mph at Friona (Parmer County).
The local office's own words before the first event, as it sent them, from the Iowa Environmental Mesonet's archive of National Weather Service text.
NWS Lubbock, TX wrote its last area forecast discussion before the first event at May 28, 12:30 PM CST, 55 minutes earlier.
Area Forecast Discussion National Weather Service Lubbock TX 130 PM CDT Tue May 28 2024 ...New SHORT TERM, LONG TERM... .SHORT TERM... (This evening through Wednesday) Issued at 119 PM CDT Tue May 28 2024 17Z upper air analysis reveals a low-amplitude, shortwave trough pivoting over the Desert Southwest and northern Mexico, with the leading edge of the geopotential height falls nosing into central New Mexico. This feature was translating through a larger-scale, mid/upper-level ridge, which is currently centered over the Rocky Mountains; and a dampened, mid-level jet streak near 35 kt was rounding the base of this low-amplitude trough as it emerges into western Texas. Mid-level, isentropic ascent is already present as evident by the shallow field of altocumulus floccus advecting eastward over the CWA. At the surface, a weak, lee cyclone was analyzed near ROW, with the dryline extending to its south and a quasi-stationary front branching eastward into the South Plains and into the vicinity of LBB, before bending southeastward into the southern Rolling Plains and northern Permian Basin. This stalled front has become convectively-reinforced by a well-defined outflow boundary generated by an MCS earlier this morning along the Upper Red River Valley, and trends in visible satellite and West Texas Mesonet (WTM) data indicate that the airmass in wake of this outflow continues to recover. WSR-88D data also detects multiple waves with this outflow boundary as it propagates westward, but it appears that the waves are dissipating in amplitude as pressure tendencies have risen 1 mb in the past hour as diabatic heating intensifies and the forward-speed diminishes as it interacts with the front. The differential heating associated with the passage of this outflow, and the presence of the stalled front, has resulted in surface temperatures breaching 90 degrees within the airmass across locations along the HWY-385 corridor, while surface temperatures remain in the middle-upper 70s across the Rolling Plains. WTM data also indicates a corridor of mid-60 degree dewpoints advecting northwestward along the theta-e gradient in the immediate vicinity of the quasi-stationary front. Explosive thunderstorm development is expected to occur this afternoon near the triple point in the South Plains, where a tongue of high theta-e air will continue to advect towards the surface low (this is currently and has been evident on WTM data for the last several hours). The 12Z RAOBs from WFO AMA and MAF observed MUCAPE values between 1,500-3,000 J/kg amongst steep, mid-level lapse rates between 8.8-9.4 deg C/km. Gradual, geopotential height falls, in addition to intense, diabatic surface heating, should bolster both mixed-layer CAPE values to >=2,500 J/kg across the Caprock this afternoon amidst effective shear magnitudes approaching 50 kt as the backed, southeasterly winds near 20-30 kt enhance the component of low-level storm-relative inflow beneath the 250 mb jet streak at around 50 kt. The convective reinforcement of the quasi-stationary front juxtaposed to the belt of 20+ kt southeasterly flow will result in an enhanced corridor of streamwise vorticity within the inflow-layer, with storms rapidly becoming supercellular and discrete propagation is expected as cells move near or along the quasi-stationary front. LCLs will lower substantially as cells move southeastward, and the ingestion of buoyant, high theta-e air; and solenoidal flow along the stalled front is expected to result in an initial threat for tornadoes, some of which could be rain-wrapped and significant (i.e., capable of producing EF2+ damage), especially along and west of the I-27 corridor. Supercells will also pose a high threat for very large hail between 2-3 inches in diameter, and potentially wide, bulbous downdrafts will augment the potential for wind-damage with gusts to 80 mph possible. The cold pools associated with potentially multiple supercells are expected to result in upscale growth towards the evening across the South Plains, with several swaths of 60-70 mph wind gusts and isolated significant wind gusts between 75-85 mph possible as the magnitude of downdrafts generate intense theta perturbations. A forward-propagating MCS may materialize as the environment for MCS maintenance remains unsupportive of back-building via anti-parallel Corfidi vectors with a downshear component in excess of 40 kt. Flash flooding will be possible from rain rates of 2+"/hr, but the fast system motion will mitigate more-widespread flooding concerns. The MCS/cluster of supercells is forecast to move southeastward this evening and tonight as it progresses into the Rolling Plains, and the potential exists for meso-beta-scale vortices to develop should mesocyclones remain embedded within the MCS, which would maintain the potential for significant (>=75 mph) wind gusts. The system is forecast to clear the CWA near midnight CDT, with prevailing winds remaining out of the east-southeast across the northern periphery of the stalled front as it moves into the northern Permian Basin. Low stratus will develop as the lower portions of the airmass reach saturation as a backed, low-level jet remains positioned over the CWA with temperatures falling into the upper 50s and lower 60s tomorrow morning. Sincavage && .LONG TERM... (Wednesday night through next Monday) Issued at 119 PM CDT Tue May 28 2024 Barring some remnant elevated convection Wednesday morning, the remainder of the day is looking very stable under widespread low clouds and moist easterly flow that backs all the way into NM. Some thinning to this stratus is likely through the afternoon, yet limited windows for strong heating should keep a hefty cap intact and close the door to additional storms. Feel the global models are overblown with QPF off the Caprock through the afternoon given such muted forcing in continued semi-zonal flow, so NBM's PoPs were trimmed lower and kept more in line with the drier CAMs. This story changes by Thursday as a shortwave trough turns our flow aloft more cyclonic and a modest upper jet streak noses over the South Plains. This improved flow is forecast to nudge a weak surface low and dryline out of NM before stalling from the western TX PH through the western South Plains by peak heating. Models still differ on various factors to these boundaries - the greatest of which may involve an outflow-enhanced cold front diving south from the TX PH through the day which would throw a monkey wrench into storm chances and even high temps. Provided low clouds ahead of the dryline can erode, the lid should be breakable by late afternoon especially as the shortwave trough draws closer. Severe storms are certainly on the table with all modes possible yet again. Storm chances trend lower by Friday in the wake of the shortwave trough, although this is not reflected well by the NBM which depicts likely PoPs at times which has poor support from the latest models. Opted to undercut NBM's PoPs for Friday mainly given the overarching theme of subsidence which should overturn by Saturday as the next shortwave trough arrives in westerly flow. Models and ensembles are in surprisingly good agreement with Saturday's precip chances and an overall weak cap, so this may be our final hurrah for rain chances before a tall dome of high pressure sets its sights on West Texas early next week complete with a return to hotter temps. && .AVIATION... (18Z TAFS) Issued at 1217 PM CDT Tue May 28 2024 Severe thunderstorms are expected to affect KCDS, KLBB, and KPVW, this afternoon and evening. Surface wind gusts near 50 kt and very large hail in excess of two inches in diameter surface-to-aloft will accompany the severe storms. TEMPO groups were assigned to all terminals but adjustments to timing may be required. Storm chances will end from northwest-to-southeast tonight with the prevailing wind remaining out of the southeast and east. MVFR CIGs will develop tomorrow morning at all terminals and last through the end of the TAF period. Sincavage && .LUB WATCHES/WARNINGS/ADVISORIES... None. && SHORT TERM...09 LONG TERM....93 AVIATION...09
Hazardous Weather Outlook...UPDATED National Weather Service Lubbock TX 1106 AM CDT Tue May 28 2024 TXZ021>044-291615- Parmer-Castro-Swisher-Briscoe-Hall-Childress-Bailey-Lamb-Hale-Floyd- Motley-Cottle-Cochran-Hockley-Lubbock-Crosby-Dickens-King-Yoakum- Terry-Lynn-Garza-Kent-Stonewall- 1106 AM CDT Tue May 28 2024 This Hazardous Weather Outlook is for the South Plains, Rolling Plains, and the far Southern Texas Panhandle. .DAY ONE...This afternoon and tonight. Severe thunderstorms will develop this afternoon and persist through the evening hours. The primary hazards will include very large hail to the size of baseballs, damaging wind gusts up to 80 mph, and a few tornadoes, especially along the Interstate 27 corridor. Flash flooding will also accompany storms this afternoon and evening. .DAYS TWO THROUGH SEVEN...Wednesday through Monday. Severe thunderstorm chances are forecast to increase on Thursday. All hazards will be possible, including: damaging winds, very large hail, although unlikely a tornado or two cannot be ruled out. The potential for severe weather remains in the forecast heading into the weekend. .SPOTTER INFORMATION STATEMENT... Spotter activation will likely be needed.
The Lubbock radar (KLBB), 88 km away, was scanning. The volume nearest the first event began at 19:25 UTC.
18 hail, 4 high wind, 4 thunderstorm wind. Local standard time, as filed.
The Southwest Cotton Growers in Wellman reported quarter size hail that lasted for ten minutes.
Multiple storm chasers reported a swath of hail approximately seven to nine miles northwest of Needmore. Hail ranged in sizes from golf ball size to tennis ball size. No damage was reported.
A storm chaser reported ping pong ball size hail just to the southwest of Friona.
Several storm chasers reported hail along Texas State Highway 214 south of Enochs. Reported hail ranged in size from half dollar to two inches in diameter. No damage was reported.
A storm chaser reported half dollar size hail south of Sundown along Farm to Market Road 303.
Numerous storm chasers reported a swath of hail ranging in size from golf balls up to three inches in diameter. No damage was reported.
Several storm chasers reported a swath of hail east of Meadow ranging in size from golf ball to baseball size. No damage was reported.
A storm chaser reported golf ball size hail north of Whitharral along US Highway 385.
A storm chaser reported half dollar size hail along Farm to Market Road 179 southwest of New Home.
A report from the public was received of quarter size hail in Anton.
Numerous storm chasers reported a long lived swath of giant hail from approximately eight miles south of Pep through three miles south of Smyer. Near the beginning of this swath of hail along Farm to Market 303 near Petit, a storm chaser relayed a video of hail that measured five inches in diameter. Hail ranging in size from two to three inches in diameter substantially affected the city of Levelland causing extensive damage.
Storm chasers and an NWS cooperative weather observer observed a swath of hail ranging in size from quarters to baseballs from approximately three miles west of Tahoka into the city of Tahoka.
Storm chasers reported a swath of hail north of Morton with sizes ranging from quarters to two inches in diameter. No damage was reported.
Numerous reports were received of a swath of hail in and around Wolfforth ranging from the size of peas to golf balls.
A storm chaser reported golf ball size hail west of Wilson.
A Texas Tech University West Texas mesonet site near Morton measured severe wind gusts from 2354 CST through 2355 CST. A peak wind gust of 62 mph was measured at 2354 CST.
An NWS storm survey team observed damage to utility poles, trees, and center pivots in and around Levelland. Damage escalated in both coverage and intensity east of US Highway 385 with a concentrated area of damage noted in and around Kauffman Park. Here, winds of 90 mph to 120 mph caused partial failures to some roofs and completely destroyed several wooden outbuildings. Many homes and vehicles|suffered broken windows with roughly one dozen trees uprooted. One home lost roughly 30 percent of its roof and insulation while a wooden framed workshop in its backyard was completely destroyed and|blown two homes away. Numerous wooden and metal fences were also heavily damaged or destroyed. The Penny Newman cotton gin on the east side of Levelland suffered total destruction from winds estimated around 110 mph.
A public report was received of quarter size hail west of Ropesville.
A Texas Tech University West Texas mesonet site near Wolfforth measured severe wind gusts from 0117 CST through 0118 CST. A peak wind gust of 59 mph was measured at 0117 CST.
A Texas Tech University West Texas mesonet site near Tahoka measured severe wind gusts from 0153 CST through 0202 CST. A peak wind gust of 95 mph was measured at 0156 CST. A storm survey team|observed 20 center pivots flipped over and damaged along with several newly installed power poles primarily on the north and east sides of Tahoka. In Tahoka, damage was relegated to some uprooted trees and numerous fallen tree limbs, with some minor structural damage noted to roofs and siding. No additional damage indicators were available beyond US Highway 380 and County Road Y east of Tahoka.
After NWS Directive 10-1605, the rules offices file Storm Data by.
Every storm in Texas in 2024Every state in 2024This day in weather historyWarnings in Texas, May 2024
NOAA National Centers for Environmental Information, Storm Events Database, compiled from the National Weather Service’s monthly Storm Data. Complete through 2026-06; NCEI adds each month about 75 days after it ends and revises past years a few times a year. Rebuilt 2026-09-24. Each event’s entry at NCEI: 1171363, 1171366, 1171369, 1171370, 1171373, 1171376, 1171381, 1171382, 1171385, 1171386, 1171388, 1171390, 1171393, 1171396, 1171397, 1171399, 1171398, 1171400, 1171401, 1171402, 1171403, 1171404, 1171408, 1171405, 1171406, 1171407.