During the evening hours of March 28, 2000, an intense F3 tornado struck Downtown Fort Worth, Texas, causing significant damage to numerous buildings and skyscrapers as well as two deaths. The tornado was part of a larger severe weather outbreak that caused widespread storms across Texas and Oklahoma in late-March, spurred primarily by the moist and unstable atmospheric environment over the South Central United States as a result of an eastward-moving upper-level low and shortwave trough. The tornado outbreak was well forecast by both computer forecast models and the National Weather Service, though the eventual focal point for the severe weather—North Texas—only came into focus on March 28 as the conditions favorable for tornadic development quickly took hold.

The tornado initially began as a relatively weak tornado in River Oaks, gradually strengthening as it tracked southeastward and then eastward towards Fort Worth's central business district. The twister damaged 266 homes across its long and wide path, out of which 28 were destroyed. Damage surveys indicated that much of the tornado's destruction was due to structural deficiencies in many of the older subdivisions impacted by the tornado. Various high-rise and low-rise buildings in downtown Fort Worth sustained various degrees of structural damage including numerous broken windows. Nine other tornadoes also occurred across North Texas on March 28; although most were relatively inconsequential, another strong F3 tornado struck portions of Arlington, including Arlington Municipal Airport. Aside from the two deaths caused by the tornado, a third person was killed in north Fort Worth by a fall of baseball-sized hail.

Meteorological synopsis

Early on March 28, an upper-level low tracked eastward into the Southern United States along with its associated shortwave trough, sending the subtropical jet through Texas and bringing along with it strong west-northwesterly winds in the upper-levels of the troposphere. Concurrently, a cold front extended zonally tracked south across the Great Plains before eventually stalling near the Red River valley, providing an additional focus area for storm development. Favorable conditions for severe weather were expected ahead of the upper-level low over areas of North Texas; accordingly, the Storm Prediction Center (SPC) issued a moderate risk for severe weather for the region, citing an unstable atmosphere caused by steep lapse rates of 7.5-8.0 °C/km and high convective available potential energy values. The environment was expected to be conducive for the development of supercells as the warped subtropical jet produced strong wind shear over Texas.

Later that day, a low-level low-pressure area developed west of Wichita Falls at the intersection of a dry line extended southward across Central Texas and the stationary front extended eastward across the Red River valley. With the low-pressure system now in place, the air mass over the Red River valley became increasingly unstable, featuring surface temperatures near and high dew points caused by the northerly surge of moisture induced by the subtropical jet. The combination of high temperatures and a moist atmosphere resulted in a favorable environment for thunderstorm development. However, despite the heat, temperatures alone were insufficient in breaking the capping inversion–an area of warmer air aloft that prevents the relativity cooler air near the surface from rising. Instead, the approaching shortwave trough provided the impetus necessary to force convection to occur, allowing for the formation of showers and thunderstorms.

Initially, computer models indicated that the day's storms would primarily feature strong winds and hail with a minimal risk for tornadoes, with severe weather occurring mainly north of the stalled front in Oklahoma. However, conditions improved further than expected, leading the National Weather Service Weather Forecast Office in Fort Worth, Texas to intensify its verbiage in its public forecasting products as the day progressed and highlighting areas around the Dallas–Fort Worth metroplex as potential risk areas for tornadoes. Thunderstorms began to develop earnestly along the dry line as the afternoon progressed, beginning with initial storm development northeast of Abilene. The strong southwesterly winds aloft from the curved subtropical jet over the region helped to ventilate the storms, allowing for their persistence and intensity. The SPC issued its first of two tornado watches for the event at 2:53 p.m. CST (20:53 UTC) for portions of southern Oklahoma and North-Central Texas. The most favorable environment for tornadoes was initially over the Red River but shifted southward to include the Dallas–Fort Worth area in the evening hours. As storms continued to develop along a line paralleling Interstate 35, some storms congealed into a mesoscale convective system near the Metroplex; this cluster of storms produced both F3 tornadoes in Fort Worth and Arlington. The complex of storms eventually evolved into a transient bow echo that continued to track eastward into Louisiana. Elsewhere, supercells continued to propagate eastward across North and South-Central Texas along the dry line, slowly weakening after sunset.

Confirmed tornadoes

March 28 event + List of confirmed tornadoes – Tuesday, March 28, 2000F#LocationCounty / parishStateStart coord.Time (CST)Path lengthMax widthSummary F0St. JoMontagueTX17:24A mobile home was damaged in St. Jo. Hail from the same supercell damaged cars on US 82. The same storm would later produce several funnel clouds and an additional tornado over Cooke County. F3Fort WorthTarrantTX18:18–18:282 deaths – See above section on this tornado – 80 people were injured. F0ItascaHillTX18:20This brief tornado did no damage. The same thunderstorm would later spawn two additional tornadoes in Navarro County. F0LindsayCookeTX18:20This brief tornado did no damage. The same storm also produced the earlier F0 tornado in Montague County, in addition to several funnel clouds. F3ArlingtonTarrant, DallasTX19:05–19:15After the Fort Worth tornado dissipated, another thunderstorm developed over Johnson County, tracking northeastward into Tarrant County and eventually merging with the supercell that had produced the earlier F3 tornado. The new development prompted the re-issuance of the tornado warning for Tarrant County at 6:40 p.m. CST (00:40 UTC). The Arlington tornado touched down then touched down 25 minutes later, causing initial damage to a restaurant; the tornado's touchdown coincided with the appearance of a tornado vortex signature on radar imagery. Well-built homes within a residential area sustained widespread damage, with some houses experiencing up to F3-rated damage; such damage occurred after garage doors failed, allowing tornadic winds to unroof homes and push out exterior walls. As a consequence, homes that faced the tornadic winds sustained more damage than homes whose attached garages were sheltered from the strong winds. The tornado then did additional damage to one- and two-story homes in another subdivision, producing F3 damage. Many homes suffered the collapse of brick masonry walls due to poor construction as they were not properly anchored to the homes' frames. The tornado then swept across northern portions of the Arlington Municipal Airport, dealing F2 damage before briefly paralleling I-20. The tornado then crossed the interstate, overturning at least one 18-wheeler. The tornado continued to track northeast, causing F2 damage to a subdivision northeast of Grand Prairie Municipal Airport in Dallas County before dissipating. F0Leon ValleyBexarTX19:11–19:12This small and short-lived tornado did minimal damage. However, the tornado was preceded by winds and large hail that damaged cars in Leon Valley. F0RoaneNavarroTX19:55A barn was destroyed, and another was unroofed by the tornado, causing $10,000 in damage. The same storm that produced this tornado also produced an F1 tornado near Bazette and produced the earlier tornado in Hill County, in addition to widespread non-tornadic damage. F0WSW of WilmerDallasTX19:55Storm spotters observed a brief touchdown in rural areas of Red Oak and Wilmer from the same supercell that spawned the earlier F3 tornado in Arlington. F1BazetteNavarroTX20:15Three mobile homes and five barns were destroyed in Bazette. The roofs of two other homes were damaged. Damage from this tornado amounted to $200,000. F0TrinidadHendersonTX20:30A few residences in Trinidad sustained minor damage and trees were downed. The same parent thunderstorm spawned the tornadoes in Navarro and Hill counties and also produced destructive hail over nearby Malakoff and Athens.

Fort Worth, Texas

The thunderstorm that would eventually produce this intense and destructive F3 tornado in Fort Worth developed from a cluster of storms that formed west of the city. At 4:38 p.m. CST (22:38 UTC), a severe thunderstorm warning was issued on the quickly organizing storm for Parker County. About an hour later, another severe thunderstorm warning was issued, this time for Tarrant County, as the storm continued to track eastward. Radar imagery showed that the supercell was rapidly organizing, developing a bounded weak echo region and hook echo—radar signatures that hint at a strong and potentially tornadic thunderstorm—in less than a half-hour. Radar also indicated that a broad mesocyclone had developed by around 6:00 p.m. CST (00:00 UTC), extending vertically through the entirety of the supercell. At around the same time, a wall cloud was spotted in association with the rotating thunderstorm while baseball-sized hail fell ahead of the rotation in northern Fort Worth along I-820. Winds from the downdraft of another small thunderstorm south of Fort Worth allowed the strengthening supercell to organize further. At 6:10 p.m. (00:10 UTC), a tornado warning was issued for Tarrant County, and accordingly emergency sirens were activated in the Fort Worth a minute later.The tornado touched down at 6:18 p.m. CST (00:18 UTC) near Castleberry High School northwest of downtown Fort Worth. Initially, the tornado lacked a condensation funnel, and could only be visually identified as dust swirls near the ground beneath the rotating wall cloud aloft; the tornado maintained this appearance for the first five minutes of its lifespan, after which a condensation funnel eventually developed. The first signs of damage occurred in the River Oaks area along SH 183 where metal roof panels were stripped off of a vacant fast food restaurant. After crossing the highway, the tornado inflicted sporadic F0 damage to an older residential area, breaking tree branches and causing some damage to outbuildings; a few chimneys were toppled off of homes. At the time, the tornado's damage path was only a few hundred feet wide. A roof of a home near Roberts Cut Off Road was partially removed, signifying the first instance of F1 damage. Several large and rotted trees were uprooted by the tornado's strong winds as it moved through the area. The tornado then passed directly over Castleberry High School, causing significant damage to the school's field house. Tornadic debris—including rooftop air conditioning units, gravel, and other detached construction—was thrown by the tornado at the school's western façade, causing minor damage. Throughout River Oak, three homes sustained major damage while 51 others experienced minor damage.