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October 26, 2010 · Limestone County · 2010
EF0

October 26, 2010

2:40 PM
Limestone County, Alabama · Near Madison (ZIP 35756)
Fatalities
0
Injuries
0
Path Length
0.3 mi
Max Width
50 yd
DateOctober 26, 2010
Time2:40 PM
CountyLimestone
CityMadison
Property Loss$5000.00M
Crop Loss$0
SourceNCEI 259755
NWS Birmingham

1.9 S Greenbrier - 1.8 SSE Greenbrier An EF-0 tornado with peak winds up to 70 mph touched down very briefly along Greenbrier Road north of the of the Interstate 565 interchange. The tornado uprooted several small trees and snapped several large tree limbs. Start: 34.6431/-86.8463 End: 34.645/-86.8418

NWS EF Scale: F0

Event Narrative

An EF-0 tornado with peak winds up to 70 mph touched down very briefly along Greenbrier Road north of the of the Interstate 565 interchange. The tornado uprooted several small trees and snapped several large tree limbs.

Episode Narrative

A potent upper level trough of low pressure and strong upper jet streak pushed through the Tennessee Valley on the 26th. Unseasonably high temperatures in the upper 70s to lower 80s and dew points in the upper 60s to near 70 produced an unstable environment. Deep layer shear was sufficient for supercell thunderstorms, while low level shear was quite strong as well. As a result, numerous supercell thunderstorms, many of them low topped, erupted in multiple bands across northern Alabama as early as late morning and lasted into the early evening hours. The storms brought the potential for severe weather for around eight hours. Many of the storms contained meso-cyclones, but only four produced brief weak tornadoes. Others produced wind damage associated with the rear flank downdrafts of the storms or with bowing segments.

Outbreak Context

Part of 5-tornado outbreak on October 26, 2010

Shared Episode Narrative

A potent upper level trough of low pressure and strong upper jet streak pushed through the Tennessee Valley on the 26th. Unseasonably high temperatures in the upper 70s to lower 80s and dew points in the upper 60s to near 70 produced an unstable environment. Deep layer shear was sufficient for supercell thunderstorms, while low level shear was quite strong as well. As a result, numerous supercell thunderstorms, many of them low topped, erupted in multiple bands across northern Alabama as early as late morning and lasted into the early evening hours. The storms brought the potential for severe weather for around eight hours. Many of the storms contained meso-cyclones, but only four produced brief weak tornadoes. Others produced wind damage associated with the rear flank downdrafts of the storms or with bowing segments.

Source Data
NCEI Event ID: 259755
SWDI Tornado ID: 2010-10-26T20:35:26Z_KHTX_P8
SWDI Radar Site: KHTX
SWDI Signature: TVS

See Also

0.3 mi50 yd wide