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1999 Bridge Creek–Moore tornado

F5 tornado in Oklahoma, U.S.

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The May 3, 1999 Moore F5 tornado that killed over 30 people in the Oklahoma City suburbs. While the Flickr license does not allow commercial use, all NOAA/NSSL images are legally in the public domain.
Mike Eilts, National Severe Storms Laboratory · Public domain

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The tornado first touched down at 6:23 p.m. Central Daylight Time (CDT) in Grady County, roughly two miles (3.2 km) south-southwest of the town of Amber. It quickly intensified into a violent F4, and gradually reached F5 status after traveling 6.5 miles (10.5 km), at which time it struck the town of Bridge Creek, where parts of the community were rendered unrecognizable. It fluctuated in strength, ranging from F2 to F5 status before it crossed into Cleveland County where it reached F5 intensity for a third time shortly before entering the city of Moore. By 7:30 p.m., the tornado crossed into Oklahoma County and battered southeastern Oklahoma City, Del City, and Midwest City before dissipating around 7:48 p.m. just outside Midwest City. The greatest impacts from the tornado occurred near peak intensity in the densely populated southern suburbs and exurbs of the Oklahoma City metropolitan area. A total of 8,132 homes, 1,041 apartments, 260 businesses, eleven public buildings, and seven churches were damaged or destroyed.

Large-scale search and rescue operations immediately took place in the affected areas. A major disaster declaration was signed by President Bill Clinton the following day (May 4) allowing the state to receive federal aid. In the following months, disaster aid amounted to $67.8 million. Reconstruction projects in subsequent years led to a safer, tornado-ready community. On May 20, 2013, nearby areas adjacent to the 1999 storm's track were again devastated by another large and violent EF5 tornado, resulting in 24 fatalities and extreme damage in the South Oklahoma City/Moore area.

Meteorological synopsis

The Bridge Creek–Moore tornado was part of a much larger outbreak which produced 71 tornadoes across five states throughout the Central Plains on May 3 alone, along with an additional 25 that touched down a day later in some of the areas affected by the previous day's activity (some of which were spawned by supercells that developed on the evening of May 3), stretching eastward to the Mississippi River Valley. The most prolific tornadic activity associated with the May 3 outbreak – and the multi-day outbreak as a whole – occurred in Oklahoma; 14 of the 66 tornadoes that occurred within the state that afternoon and evening produced damage consistent with the Fujita scale's "strong" (F2–F3) and "violent" (F4–F5) categories, which, in addition to the areas struck by the Bridge Creek–Moore tornado family, affected towns such as Mulhall, Cimarron City, Dover, Choctaw and Stroud.

Setup

The outbreak was caused by a vigorous upper-level trough that moved into the Central and Southern Plains states on the morning of May 3. That morning, low stratus clouds overspread much of Oklahoma, with clear skies along and west of a dry line located from Gage to Childress, Texas. Air temperatures at 7:00 a.m. Central Daylight Time ranged in the mid to upper 60s °F (upper 10s to near 20 °C) across the region, while dew point values ranged in the low to mid 60s °F (mid to upper 10s °C). The Storm Prediction Center (SPC) in Norman, Oklahoma, a division of the National Weather Service, initially issued a slight risk of severe thunderstorms early that morning stretching from the Kansas-Nebraska border to parts of southern Texas, with an intended threat of large hail, damaging winds and tornadoes. By late morning, the low cloud cover began to dissipate in advance of the dry line, but during the afternoon high cirrus clouds overspread the region, resulting in filtered sunshine in some areas that caused atmospheric destabilization. The sunshine and heating, combined with abundant low-level moisture, combined to produce a very unstable air mass. Upper air balloon soundings observed strong directional wind shear, cooling temperatures at high atmospheric levels, and the increased potential of CAPE values potentially exceeding 4000 J/kg, levels that are considered favorable for supercells and tornadoes.

Forecast and initiation

As observations and forecasts began to indicate an increasing likelihood of widespread severe weather conditions even more favorable for strong tornadoes, the SPC issued a moderate risk of severe weather at 11:15 a.m. CDT for portions of Kansas, Oklahoma and Texas along and near the Interstate 40 corridor.

... N CENTRAL TX/OK/SRN KS ...

LOW LEVEL JET WILL MAINTAIN SIGNIFICANT INFLOW OF LOW LEVEL MOISTURE WITH SURFACE DEWPOINTS AROUND 65F. CLEARING SKIES EVIDENT ON VISIBLE IMAGES WILL FURTHER CONTRIBUTE TO STRONG DESTABILIZATION OVER REGION WITH LATE AFTERNOON MUCAPES FORECASTED FROM 3500 TO 4500 J/KG OVER MDT RISK AREA. AS SHORT WAVE APPROACHES WRN OK/TX BORDER…LIFTING WILL DEEPEN NEAR/ALONG DRYLINE WITH THUNDERSTORMS INCREASING AS THEY MOVE EWD INTO INSTABILITY AXIS. 50 KT MID LEVEL SWLY FLOW SPREADING OVER LOW LEVEL JET AXIS WILL PROVIDE SUFFICIENT SHEAR FOR A FEW STRONG OR VIOLENT TORNADIC SUPERCELLS GIVEN THE ABUNDANT LOW LEVEL MOISTURE AND THE HIGH INSTABILITY.

— NWS Storm Prediction Center (SPC), May 3, 1999 1630 UTC Day 1 Convective Outlook

At 3:49 p.m. CDT, the SPC − having gathered enough data to surmise that there was a credible threat of a significant severe weather outbreak occurring within the next few hours − amended its Day 1 Convective Outlook to place the western nine-tenths of the main body of Oklahoma, central and south-central Kansas and the northern two-thirds of Texas under a high severe weather risk, denoting a higher than normal probability of strong (F2+) tornadoes within the risk area. About 40 minutes after the revised outlook's issuance, at 4:30 p.m. CDT, the SPC issued a tornado watch for western and central Oklahoma, effective from 4:45 p.m. until 10:00 p.m. CDT that evening, for the threat of tornadoes, hail up to three inches (7.6 cm) in diameter, wind gusts to 80 mph (130 km/h) and intense lightning. As that happened, the first thunderstorm cell of the unfolding event had already formed over southwestern Oklahoma.

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