February 28, 2011
5:05 PM1.1 SW Pine Level - 1.3 SW North Elmore The tornado touched down just to the west of Interstate 65 near the intersection of CR 40 West and Davies Drive. The tornado tracked to the southeast over Interstate 65 and lifted just to the northwest of the town of Elmore, near the end of Dozier Farm Road. Along the path, numerous softwood trees were either snapped or uprooted. The most significant damage occurred on Harris Road where dozens of trees were snapped and uprooted. There was partial roof damage to numerous homes in the same area and a single-wide mobile home was overturned. Start: 32.5699/-86.4 85 4 End: 32.5546/-86.3329
NWS EF Scale: F0
A tornado touched down 1.5 miles southwest of Pine Level in Autauga County and tracked southeastward for 4.28 miles before exiting Autauga County about 0.36 miles north of Kenner Creek, south southwest of Deatsville, at 1710CST. This tornado continued into Elmore County for another 4.5 miles, before dissipating at 1720CST. In Autuaga County, numerous trees were snapped or uprooted and several homes sustained minor shingle or soffit damage. One mobile home sustained significant roof damage.
On the afternoon of Sunday, February 27th, a low pressure system developed in the Southern Plains, eventually tracking across the Tennessee Valley, well to the north of Alabama. In response to this low pressure, coupled by high pressure off the Atlantic Coast, southerly flow brought low 60 dew point temperatures as far north as Huntsville by 12 am Sunday night. By the late morning hours of Monday, February 28th, a secondary surface low developed and tracked across the northern half of the state of Alabama. This surface low created storms that began of a cellular nature by Noon on Monday. These cells evolved into a broken line of thunderstorms by the middle of the afternoon on Monday. Embedded in the line were storms that developed supercellular structures, a few of which spawned tornadoes and many areas of straight line wind damage. Click on each for a summary of the tornadoes.
Part of 5-tornado outbreak on February 28, 2011
On the afternoon of Sunday, February 27th, a low pressure system developed in the Southern Plains, eventually tracking across the Tennessee Valley, well to the north of Alabama. In response to this low pressure, coupled by high pressure off the Atlantic Coast, southerly flow brought low 60 dew point temperatures as far north as Huntsville by 12 am Sunday night. By the late morning hours of Monday, February 28th, a secondary surface low developed and tracked across the northern half of the state of Alabama. This surface low created storms that began of a cellular nature by Noon on Monday. These cells evolved into a broken line of thunderstorms by the middle of the afternoon on Monday. Embedded in the line were storms that developed supercellular structures, a few of which spawned tornadoes and many areas of straight line wind damage. Click on each for a summary of the tornadoes.