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EF0 tornado in Fauquier County, Virginia

Tornado April 6, 2017 · Fauquier County, Virginia

EF0
Rating
0.9 mi
Path length
50 yd
Path width
EF0EF1EF2EF3EF4EF5Unrated

The path drawn at its surveyed width of 50 yards (0.03 mi) — zoom in and the swath grows to true scale. Other tornadoes recorded nearby that day are shown faint.

What EF0 means. On the Enhanced Fujita scale, EF0 is light damage: shingles and siding peeled, gutters torn, branches broken, consistent with estimated gusts of 65–85 mph. The rating comes from a survey of the worst damage after the storm, not from a wind measurement, so it says as much about what the tornado hit as about how strong it was.

What the National Weather Service wrote

The National Weather Service in Baltimore MD/Washington DC has

confirmed a tornado southwest of Warrenton in Fauquier County

Virginia on April 6, 2017.

An extensive area of tree damage was noted along a several mile long

path in west-central Fauquier County. Embedded within this straight-

line wind damage was a small concentrated area of convergent tree

damage consistent with an EF-0 tornado.

A row of trees just north of Harts Mill Road was blown down towards

the west-northwest, while several other trees just south of the road

were snapped and fell towards the northeast. A similar pattern of tree

damage was found at a residence on Woodbourne Lane a quarter mile to

the northeast, where several dozen hardwood trees were uprooted, mainly

falling towards the east but a couple fell towards the west.

Further southwest and to the northeast of the tornadic damage,

hardwood and softwood trees were snapped and uprooted but all falling

to the northeast over a nearly mile-wide swath, indicating straight-line

wind damage. It is notable that the straight-line wind damage was more

severe than that caused by the brief tornado.

The National Weather Service would like to thank the Fauquier County

Emergency Management Agency and the residents interviewed for their

assistance in this survey.

The wider storm

Cutoff low pressure was over the Ohio Valley. Another area of low pressure strengthened overhead on the occluded boundary. Warm and moist air from the south lead to an unstable atmosphere. Strong shear profiles were in place due to the cutoff low to the west. Strong lift associated with the developing low combined with strong shear and enough instability to produce severe thunderstorms and isolated tornadoes.

Began near Turnbull (38.6746, -77.8656).

Other tornadoes from the same storm system

5 more tornadoes the National Weather Service filed under this storm episode.

Source: NOAA Storm Events Database, event 691223. Narratives are written by the National Weather Service forecast office that issued the report.

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