May 3, 2003 (2003-05-03)-May 11, 2003 (2003-05-11) Highest winds Tornadic: 180 mph (290 km/h) in Perryville, Missouri Non-tornadic: 115 mph (185 km/h) in Wayne County, Kentucky(estimated); 105 mph (169 km/h) in Johnson County, Missouri(measured) Tornadoes confirmed 363 tornadoes (62 significant)[note 1] Max.rating1 F4tornado Duration of Stockton, UT. [150] Another cluster of potentially severe thunderstorms formed along the Ohio River in the early afternoon in the wake of the storms that moved through West Virginia, and additional storms continued to form in the region through the afternoon and evening in the vicinity of a well-defined warm front. High F-1 damage was observed about one-half mile west of Mohawk Corner where one exterior wall was destroyed on a frame house and several barns were destroyed. [120] These potent conditions were also present as far south as Central Texas, though the stronger capping inversion farther south meant more widespread severe activity was less likely. Hundreds of trees were uprooted or snapped off as were power poles. Stockton tornado (F3) The second major tornado produced by the . Damage was consistent with an upper-end F3 here. [81], The SPC predicted a Slight Risk for a broad area of the Eastern and Central U.S. in their 06:00UTC (1:00a.m. CDT) Day1 Convective Outlook for May7. The tornado initially touched down just east of Liberal, MO in Barton County as an F-1. "The word devastation doesn't do it justice. The tornado originated from an isolated supercell thunderstorm that had developed along the dry line in northwestern Texas; the same thunderstorm produced at least three other tornadoes during its two-hour traversal of Haskell County, Texas. [254] Minor damage was inflicted to the roofs of hundreds of homes. We intercepted the F3 tornado that went near Baxter Springs, Kansas (Cherokee County) and into SW Missouri. However, the tornado quickly grew in size and intensity, causing F3damage to two homes south of Parallel Parkway near Interstate 435 and expanding to a width of over 500yd (460m). CDT). The cause of these successive troughs is unknown, but they proved a key factor in the prolonged nature of the outbreak. Tonight Mostly clear. Also noted at this point was that a compact car was picked up and flipped across the road. [245] The flooding washed out roads, damaged at least 200residential buildings, and inundated numerous businesses. A very moist and unstable airmass was located south of the front. and Three people were killed in town, and 20 others were injured. [215] Overall, the F4tornado killed two people and injured another thirty; one woman succumbed to her injuries seven months later. USGenWeb Archives--Cedar CountyJerico Springs--off site link. It took a tornado just a few minutes Sunday night to rip it all apart and devastate this Missouri Ozarks community of about 2,000. 3. Stockton, MO is a Very High Risk area for tornados. [129] The air mass to the east of the dry line was also becoming exceptionally unstable;[157] by 23:05UTC (6:05p.m. CDT), three tornado watches were in effect along a band from North Texas and central Indiana. Local Office Research With soils saturated from prior rains, the prolonged precipitation period produced seasonally anomalous runoff that flowed into creeks and rivers, resulting in rapid rises of streams and associated rivers, including Chickamauga Creek, Conasauga River, Chattahoochee River, Flint River, and Sweetwater Creek. [36] One supercell developed over northeastern Oklahoma and moved into southwestern Missouri, producing an F3tornado that struck Pierce City, Missouri. [241] Radar estimates suggested that as much as 58in (130200mm) fell in some locations in one hour. Of these, 62 reached at least F2-intensity, while 6 reached F4. [118][122] A third tornado watch was issued for northern Kansas and southern Nebraska at 18:50UTC (1:50p.m. CDT) and the air mass overhead became increasingly unstable with CAPE values over 3000J/kg ahead of a developing low-pressure area in the vicinity of Russell, Kansas. [106][107] During the day, a low-pressure area would intensify over southeastern Colorado, forcing a warm front northward from Oklahoma to Kansas and resulting in a weather pattern resembling the severe weather setup from May4. HERMLEIGH, Tex. A fairly potent spring storm delivered with . On Friday, NWS confirmed that an EF-Unknown tornado did indeed touch down in a field around 12:20 p.m. about eight miles east-southeast of Isleton in San Joaquin County. [203] According to the National Climatic Data Center, 11tornadoes touched down in Kentucky and Tennessee between 611UTC (16a.m. CDT), though a 2015 reanalysis conducted by the National Weather Service Nashville, Tennessee, found additional tornadoes that placed the total at 15. Wind Gusts 12 mph. 2. [78][79] There were 24tornadoes in Missouri, 9 in Illinois, and 9 in Kentucky between 2105UTC (4p.m.12:00a.m. CDT), including an F3tornado that struck Jackson, Missouri, and an F4tornado that took a path 33mi (53km) path through southern Illinois. ``Its like: where do you start, what do you do?. [19][35] The persistence of warm and moist air with the aid of daytime heating maintained the severe weather potential into the afternoon for the same areas. CDT). The tornado crossed Interstate 635 near mile marker 11.8, and it produced F1 damage east of this point until the tornado apparently dissipated around 4:42 p.m. Total track length of this tornado . Weather Ready Nation Ambassadors The tornado path remained unbroken through northeast Polk County. [228] Downed power lines forced the closure of roads leading to Republic, Missouri. [184], Farther west, an outflow boundary remained between St. Louis, Missouri and east-central Kansas in the wake of the thunderstorms earlier in the morning, serving as a potential region for rapid thunderstorm development. The most prolific and violent day of the outbreak was May4; 79tornadoes touched down, of which 4 reached F4-intensity. "It. [313], In 2004, The Storm Prediction Center and five National Weather Service Weather Forecast Offices were awarded the Department of Commerce Gold Medalthe highest award issued by the departmentfor "providing life-saving services during a record outbreak of tornadoes during the period of May 46, 2003."[314]. [166] A powerful shortwave trough was forecast to move out of the southwestern U.S. into the southern Great Plains during the day, dragging along a portion of the jet stream with winds exceeding 100kt (115mph, 185km/h). [229] As it moved northeast across Barton County, it uprooted numerous trees and produced F1 damage to outbuildings. Winter Weather The tornado continued its east northeast track as an F-4 as it reached the community of Franklin and caused severe and total devastation to numerous homes and buildings, and tossed heavy objects and vehicles several hundred feet. Other homes on the north side of the city also sustained significant damage before the tornado crossed the Cleveland-Oklahoma county line. The warning was in place until around. [215] The most severe damage covered a swath that included eastern parts of the college campus and areas along Excelsior Springs Road,[224] with the overall damage cost totaling $60million. Grazulis. [2][6], On April30, meteorologists at the Storm Prediction Center (SPC) noted the likelihood of a major tornado outbreak across a large area of the Central and Eastern United States for the period of May26. Tornado touches down near Stockton By ABC7 Thursday, April 12, 2012 STOCKTON, Calif. "I just heard a loud, loud noise. STOCKTON MISSOURI TORNADO MAY 4th 2003 Toads Warts 189 subscribers Subscribe 8.5K views 8 years ago On May 4, 2003, a large, destructive tornado severely damaged the city of. It has been observed that the GBVTD analysis . [30] Roughly an hour later, additional tornado watchesall classified as Particularly Dangerous Situationswere issued for parts of Arkansas, Iowa, Kansas, Missouri, Nebraska, and Oklahoma ahead of an emerging line of towering cumulus and cumulonimbus clouds spanning from southeastern Nebraska to northeastern Kansas. A Great Southern bank branch was left roofless. Numerous reports of funnel clouds were reported by National Weather Service trained spotters and Chaser as the supercell moved east across McDonald and Newton Counties before the tornado touched down about three miles east of Ritchey and west of Pierce City. [12] By 21:00UTC (4:00p.m. CDT), a line of towering cumulus and cumulonimbus clouds emerged along the dry line east of Lubbock, Texas, resulting in a focused threat area for large hail, strong wind gusts, and isolated tornadoes in southwestern Oklahoma and northwestern Texas. The issuance of such watches resulted in an average lead-time of 2hours and 3minutes for fatal tornadoes. FAA Center Weather [19] One supercell led to five tornadoes in Osage and Douglas counties in Kansas, including one F3tornado. Through most of Carl Junction it was rated a high F-2. [185] An atmospheric sounding taken over Oklahoma City at 12UTC (7a.m. CDT) indicated that a robust capping inversion was in place over the region, though satellite imagery and radar data also indicated that storms were beginning to develop vertically by around 14:17UTC (9:17a.m. [294] Some overpasses in Allen Park, Michigan were flooded after a fallen light pole cut power to a storm pump station. The weak tornado lasted. [19][166] Most of these tornadoes were spawned by nine discrete supercells that formed after 19UTC (2p.m. CDT) in western Missouri and southeastern Kansas along the dry line. Aloft, the 00 UTC, 16 May initialization of the Eta model The Ingredients for a Major Tornado Outbreak Meteorological conditions came together Sunday May 4th, 2003, to produce the major tornado outbreak across southeast Kansas and the Missouri Ozarks. [35][51] The presence of very cold air in the middle and upper levels of the troposphere facilitated another locally favorable environment for severe thunderstorms over southern and eastern Michigan after about 21:00UTC (5:00p.m. Winds at 250 mb or ~35,000 ft. were ~ 125 kts, 75 kts at 500 mb or ~18000 ft. [188], Warm and moist air also advanced north into southeastern Iowa and western Illinois ahead of the low-pressure region,[189] with conducive conditions for tornadogenesis eventually extending as far north as southern Wisconsin after 23UTC (6p.m. CDT) as the low-pressure area quickly strengthened over Iowa. [206] Warm advection led to the formation and intensification of isolated storms over New York and Pennsylvania by around 14UTC (10a.m. At another location, damage was reported to have been swept against the flow of the storm some 100 - 200 yards. The storm initially entered Dallas county near the Hickory-Polk-Dallas County line southwest of Urbana. CDT). 5. [19], Closer to the main risk region, scattered thunderstorms began to form and strengthen over northwestern Texas by around 14UTC (9a.m. CDT) in response to the advection of warm air. NWS [125] The day's first tornado in Kansas was an F0tornado that touched down in Cloud County at 20:32UTC (3:32p.m. [49] Supercell thunderstorms formed over the state within this environment by 16:00UTC (9:00.a.m. Upper level diffluence provided strong vertical lift. As severe weather shifted east across the country, another trough would cross from the Pacific to the Central United States and reignite activity. It continued the F-3 rating across the rest of its path until it lifted northeast of Battlefield. [178][179] This favorable environment for rising air continued to spread east in tandem with a shortwave trough tracking across the Ohio Valley, extending conducive conditions for thunderstorm development eastward to Virginia and North Carolina in the early afternoon. The storms were complemented by other hailstorms, albeit less significant, across the region. Stockton, KS tornado at 19:56:19 CDT. [59] Winds in the mid-levels of the troposphere were similar to the situation on May4, shaped once again by a strong storm system over the central and northern Great Plains and the overlap of fast southwesterly winds at altitude with moist air below. This statement will focus on the Newton, Lawrence, Christian and southern Greene county track. [174][175] Isolated supercells later developed in the morning over central Illinois and western Indiana, aided by strong winds in the mid-levels of the troposphere and strong wind shear in the lower-levels of the troposphere. Stockton, CA 95210 .FREEZE WARNING IN EFFECT FROM 2 AM TO 8 AM PST THURSDAY. [230] In the city, 350 structures were demolished while an additional 650 received major damage. Rated F2, the tornado caused substantial damage at William Jewell College and at locales near downtown Liberty before lifting around 5:15pm. Tornado Destroys Stockton, Mo., Downtown JIM SUHR May 5, 2003 Comments Associated Press Writer After the Civil War left this southwest Missouri town in tatters, residents rebuilt the town. [116], By 16:30UTC (12:30p.m. CDT), temperatures within the areas under the SPC's Moderate and High risk regions over the central Great Plains, central Mississippi Valley, and lower Ohio Valley warmed above 80F (27C) with dew points above 70F (21C). s-1), in the Stockton, Kansas tornado of 15 May 1999, showing a prominent wavenumber-2 feature. [173][168] These storms organized into a mesoscale convective system and tracked east towards central Illinois along and north of the warm front, later developing a mesoscale convective vortex. [19] There were two other F3tornadoes in central Tennessee, with one tracking across both Hickman and Williamson counties and the other striking parts of Rutherford County. [106][107] A more conditional risk for severe weather was predicted along a dry line over the southern Great Plains due to the presence of a capping inversion that was forecast to limit the coverage of storms. [19] The complex of storms also enhanced the advection of warm air downrange farther east, bolstering the development of thunderstorms farther east by destabilizing the local air mass. [19], Temperatures along a front in Oklahoma had risen to near 80F (27C) by 15:00UTC (10:00a.m. CDT), producing a highly unstable atmosphere marked by CAPE values ranging between 30004000J/kg and lapse rates of around 8.5 C/km.
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