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EF1 tornado in Graves County, Kentucky

Tornado April 25, 2011 · Graves County, Kentucky

EF1
Rating
15.4 mi
Whole path
225 yd
Path width
$150K
Damage as recorded

NOAA records this tornado county by county. Its path ran through Weakley County, Tennessee → Graves County; the totals above are for the whole tornado.

EF0EF1EF2EF3EF4EF5Unrated

The path drawn at its surveyed width of 225 yards (0.13 mi) — zoom in and the swath grows to true scale. Other tornadoes recorded nearby that day are shown faint.

What EF1 means. On the Enhanced Fujita scale, EF1 is moderate damage: roofs badly stripped, mobile homes pushed off foundations or overturned, windows broken, consistent with estimated gusts of 86–110 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

This tornado crossed into Graves County from Weakley County, Tennessee. The tornado initially paralleled the state line, where mainly tree damage occurred. Along Kentucky Highway 303, a home was damaged. The side porch was lifted. A gazebo and a playhouse were destroyed. A garage at the north end of the house sustained major damage. Small portions of nearby grape vines were impaled in the roof of the porch, and a stick was impaled in the house. As the tornado moved northeast, mainly tree damage occurred, with uprooted trees and large limbs down. There was some tree damage south of the path near Lynnville, which was from straight-line winds. Peak winds were estimated near 100 mph. The average path width was 75 yards.

The wider storm

A pronounced mid-level shortwave trough and associated 70 to 80 knot mid-level jet progressed northeastward from the southern Plains across Arkansas and Missouri. An associated surface low developed northeastward from southwest Missouri toward northwest Illinois. A gradual increase in the warm sector southerly low level jet occurred as the surface low deepened. Increasing vertical wind shear in the moist and unstable warm sector resulted in organized severe storms. The storms were organized into bowing lines with embedded supercell structures.

Began near Dukedom (36.5000, -88.6761).

Other tornadoes from the same storm system

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

Source: NOAA Storm Events Database, event 290446. Narratives are written by the National Weather Service forecast office that issued the report.

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