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EF2 tornado in St. Clair County, Alabama

Tornado March 19, 2018 · St. Clair County, Alabama

EF2
Rating
50.7 mi
Whole path
2,000 yd
Path width
4
Injuries
$300K
Damage as recorded

NOAA records this tornado county by county. Its path ran through St. Clair County → Etowah County → Calhoun County → Calhoun County → Cleburne County → Haralson County, Georgia; the totals above are for the whole tornado.

EF0EF1EF2EF3EF4EF5Unrated

The path drawn at its surveyed width of 2,000 yards (1.14 mi) — zoom in and the swath grows to true scale. Other tornadoes recorded nearby that day are shown faint.

What EF2 means. On the Enhanced Fujita scale, EF2 is considerable damage: roofs torn off well-built houses, mobile homes destroyed, large trees snapped or uprooted, consistent with estimated gusts of 111–135 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

National Weather Service meteorologists surveyed damage in northern St. Clair County and determined that the damage was consistent with an EF2 tornado, with maximum sustained winds near 115 mph. The tornado touched down just northeast of Ashville along Highway 411. The tornado continued east northeast and uprooted and snapped numerous pine trees. The tornado intensified as it approached the Etowah County line where structural damage became evident. One house was moved off its foundation with a complete loss of roofing materials. Stands of trees were snapped off near their bases, including both hardwoods and softwoods. The tornado then crossed Neely Henry Lake and into Etowah County.

The wider storm

Six tornadoes and hail up to 3 inches in diameter affected the northern areas of Central Alabama on the afternoon and evening hours of March 19th, with a rare PDS (Particularly Dangerous Situation) Tornado Watch issued for a large portion of Central Alabama. An environment favorable for significant severe thunderstorms developed as a low-amplitude upper-level trough moved into the region with a deepening surface low passing across far north Alabama. These two features resulted in a deep column of strong wind shear with 0-6km Bulk Shear values of 60-70 knots. Additionally, moist southerly flow, warm surface temperatures, and colder temperatures aloft yielded a moderately unstable air mass. Initially, thunderstorms were producing large to very large hail. However, the tornado threat increased in the late afternoon and evening hours as wind speeds at low levels increased with the arrival of a low-level jet.

Began near Greensport (33.8552, -86.2398).

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 746988. Narratives are written by the National Weather Service forecast office that issued the report.

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