April 6, 2016
10:32 PM| Date | April 6, 2016 |
| Time | 10:32 PM |
| County | Lee |
| City | Auburn |
| Property Loss | $0 |
| Crop Loss | $0 |
| Source | NCEI 631372 |
5 SE Auburn - 2 ESE Beauregard This tornado resulted from the same storm circulation that produced an EF-0 near The Greens Apartments toward the west. Initial damage was seen along County Road 47, between Society Hill Road and County Road 27, of which included a large downed tree, broken tree branches, and a few pieces of metal sheeting removed from an outbuilding. The tornado remained on the north side of County Road 47 for a period of time, producing additional vegetative damage. The circulation then ran along County Road 47, nearing Alabama Highway 51, where several trees were uprooted and snapped. The tornado then weakened as it moved east, dissipating at County Road 166, but still took down a few trees between Highway 51 and County Road 166. Start: 32.5400/-85.4183 End: 32.5311/-85.3385
NWS EF Scale: F0 Polygon
NWS meteorologists surveyed damage near the near The Greens Apartment Homes, south of the city of Auburn, and determined it was the result of a tornado. The first signs of tornadic damage was observed on Persimmon Drive, where several trees were uprooted. Tree branches were broken along Live Oak Drive, and two trampolines were lofted downstream. The tornado then crossed US-29 into The Greens Apartment Homes, where several trees were uprooted and snapped. Light shingle damage was observed on a few units as well. Dissipation of the tornado took place within the apartment complex near the Clubhouse.
As a strong shortwave trough approached central Alabama from the west a low level southerly jet intensified over the area. Cold air advection aloft associated with the short wave produced steep lapse rates favorable for damaging winds and large hail.|The low level jet also produced a maximum of storm-relative helicity over east Alabama during the evening hours, and enhanced the threat of tornadoes.
Part of 9-tornado outbreak on April 6, 2016
As a strong shortwave trough approached central Alabama from the west a low level southerly jet intensified over the area. Cold air advection aloft associated with the short wave produced steep lapse rates favorable for damaging winds and large hail.|The low level jet also produced a maximum of storm-relative helicity over east Alabama during the evening hours, and enhanced the threat of tornadoes.