Event Summary for Central Alabama
On the evening of February 15th, four tornadoes and damaging winds affected the southeastern portion of the NWS Birmingham forecast area.
Aloft, the area was just north of the subtropical jet at 300 MB with a neutral-tilted 500 MB trough located across the Lower Mississippi Valley. The upper trough sharpened and became more dynamic as it approached Alabama, resulting in a deepening surface low and strengthening low-level jet during the afternoon and early evening hours. At the same time, a mixture of high precipitation (HP) supercells and line segments developed and consolidated into a quasi-linear convective system (QLCS) south of Interstate 85 and east of Interstate 65. Unusually cold temperatures aloft helped to create instability despite surface temperatures mainly in the 60s and dew points in the 50s in the warm sector.
Severe weather was mainly limited to areas west of Alabama through the afternoon and became refocused farther east along and ahead of a low-level confluence band extending from southwest Alabama to the northeast. Ahead of this confluence band, a discrete supercell produced a weak tornado in eastern Montgomery County. As the QLCS became more organized, a long-track and previously tornadic supercell merged with and likely enhanced the northern end of the QLCS which spawned two tornadoes in Russell County. The QLCS continued to gain momentum and low-level convergence farther south, which resulted in a spin-up tornado in southern Pike County. Although there were no discernable tornado debris signatures, each of the three QLCS tornadoes produced narrow paths of significant damage for several miles. These non-descending circulations were likely very shallow and did not contain enough upward velocity to loft debris high enough to be detected by radar.
In addition to the tornadoes, National Weather Service meteorologists surveyed two areas of straight-line wind damage. The wind damage occurred near Goshen in eastern Pike County and near Louisville in Barbour County. More information on the wind damage can be found here.
The information contained below is the individual tornado events that occurred. The data is PRELIMINARY and may be subject to change.
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