February 21, 2014
1:56 AM| Date | February 21, 2014 |
| Time | 1:56 AM |
| County | St. Clair |
| City | Moody |
| Property Loss | $0 |
| Crop Loss | $0 |
| Source | NCEI 505726 |
0.5 E Sanie - 0.7 S Odenville A tornado touched down near Jamaica Lane, west southwest of Branchville, causing minor roof damage to a mobile home and uprooting several small trees. The tornado tracked northeastward and strengthened, with winds of 85 mph, as it neared the intersection of Sanie Road and Nelsie Ann Drive. Six to eight two-story homes sustained minor roof damage as well as 30-50 trees uprooted or snapped. The tornado caused similar damage along Hurst Drive, where 25-40 trees were either snapped or uprooted and a two-story home and barn sustained minor roof damage. The tornado made a turn to the north northeast and tracked parallel to Anderson Mountain, downing trees as it crossed Copper Springs Rd near Dogwood Cir. The tornado turned to the east and continued downing trees as it crossed Shadow Bend Dr and U.S. Highway 411. The tornado track narrowed as it crossed Hwy 411 and Alabama Highway 174. The tornado downed 10-20 trees along Tucker Rd, with one down on a home. The tornado lifted just east of Tucker Road, 0.40 miles north of the intersection of Tucker Rd and Oak Ridge Dr. In addition, there was sporadic damage near the beginning and ending of this tornado path as a result of straight line winds associated with the same thunderstorm. Start: 33.6512/-86.4678 End: 33.6703/-86.4014
NWS EF Scale: F0 Polygon
A tornado touched down near Jamaica Lane, west southwest of Branchville, causing minor roof damage to a mobile home and uprooting several small trees. The tornado tracked northeastward and strengthened, with winds of 85 mph, as it neared the intersection of Sanie Road and Nelsie Ann Drive. Six to eight two-story homes sustained minor roof damage as well as 30-50 trees uprooted or snapped. The tornado caused similar damage along Hurst Drive, where 25-40 trees were either snapped or uprooted and a two-story home and barn sustained minor roof damage. The tornado made a turn to the north northeast and tracked parallel to Anderson Mountain, downing trees as it crossed Copper Springs Rd near Dogwood Cir. The tornado turned to the east and continued downing trees as it crossed Shadow Bend Dr and U.S. Highway 411. The tornado track narrowed as it crossed Hwy 411 and Alabama Highway 174. The tornado downed 10-20 trees along Tucker Rd, with one down on a home. The tornado lifted just east of Tucker Road, 0.40 miles north of the intersection of Tucker Rd and Oak Ridge Dr. In addition, there was sporadic damage near the beginning and ending of this tornado path as a result of straight line winds associated with the same thunderstorm. See other event entries for those details.
During the evening hours on Thursday, February 20, a squall line associated with a cold front moved into Central Alabama and crossed the area through the early morning hours on Friday, February 21, producing wind damage. The air mass across central Alabama was quite unstable for late February as temperatures warmed into the lower 80s across portions of the area Thursday afternoon. The expected threat was primarily damaging winds with the squall line; however, low level wind shear was supportive of tornadoes as well. The surface low, associated with the approaching cold front, moved to the northwest of the area and strengthened quickly Thursday and Thursday night. Pressure gradient winds across Central Alabama increased, resulting in localized wind damage ahead of the squall line.
Part of 2-tornado outbreak on February 21, 2014
During the evening hours on Thursday, February 20, a squall line associated with a cold front moved into Central Alabama and crossed the area through the early morning hours on Friday, February 21, producing wind damage. The air mass across central Alabama was quite unstable for late February as temperatures warmed into the lower 80s across portions of the area Thursday afternoon. The expected threat was primarily damaging winds with the squall line; however, low level wind shear was supportive of tornadoes as well. The surface low, associated with the approaching cold front, moved to the northwest of the area and strengthened quickly Thursday and Thursday night. Pressure gradient winds across Central Alabama increased, resulting in localized wind damage ahead of the squall line.