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EF1 tornado in Mobile County, Alabama

Tornado September 4, 2011 · Mobile County, Alabama

EF1
Rating
1.9 mi
Path length
100 yd
Path width
$45K
Damage as recorded
EF0EF1EF2EF3EF4EF5Unrated

The path drawn at its surveyed width of 100 yards (0.06 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

A tornado moved onshore near the mouth of East Fowl River on Byrnewood road and tracked northwest to the end of Pioneer Road in the Bellefontaine community. The tornado produced extensive damage to trees consistent with EF-1 type damage and winds between 86 MPH and 110 MPH. Four residences and one large barn had structural damage in the area between Bay Road and Pioneer Road. Of those structures, one mobile home was almost completely destroyed from a large tree that fell on it, with minor damage to mostly roofing shingles and window panes observed with the other three homes. The barn received minor structural damage on an exterior wall with three large roll-up doors completely blown out.

The wider storm

Tropical Storm Lee began as a tropical wave in the Caribbean Sea during the last week of August. By the evening of Thursday, 1 September 2011, the tropical wave further developed into Tropical Depression 13. By 1 PM the following Friday afternoon, Tropical Depression Lee had formed. Lee slowly moved northward towards the south central Louisiana coastline by Saturday afternoon 3 September, while continuing to produce extremely heavy rainfall over portions of southern Louisiana, southern Mississippi, southern Alabama and the northwest Florida Panhandle.

The outer rain-bands of Lee produced near-continuous heavy rainfall over portions of southern Alabama, southeastern Mississippi and the northwestern Florida Panhandle by early Saturday morning and that endured through early Sunday before dry air aloft wrapped into Lee's western side. The center of Lee moved over land around sunrise Sunday, 4 September. However, it would be a while before Lee would weaken to a depression because it remained nearly stationary while the southern half of the circulation was over water where it could continue to derive additional energy from the warm ocean. The next day, Lee was eventually picked up by an upper air trough, turned northeastward and resumed a faster forward speed late in the day on Sunday, 4 September as it began its welcome exit to the northeast late Sunday through late Monday.

Lee's impacts were far reaching across our region. Although the continuous rains became somewhat intermittent as dry air wrapped into Lee from the west, this created a situation from Sunday afternoon through midday Monday whereby individual thunderstorms became more intense due to increasing levels of atmospheric instability. Stronger thunderstorms and isolated tornadoes affected the North Central Gulf Coast Region, as they formed within the detached outer spiral rain-bands well to the east of Lee's center on Sunday and finally to the southeast on Monday. The highest total storm tide levels (astronomical plus surge effects) ranged from approximately 3.5 to just barely over 5 feet.

While Lee was in the process of being picked up by a fast moving upper air trough, a series of squall lines that produced moderately widespread thunderstorm wind damage along and ahead of the surface cold front, as well as more isolated tornadoes, affected the area through late Monday afternoon. In all, some 10 to 15 inches of rain fell along coastal sections of Alabama and northwest Florida. Additionally, several weak tornadoes occurred producing modest structural and tree damage. There was also moderate beach erosion and the rip currents endured over a multi-day period. Inland flooding was exacerbated along the immediate coastal zone by higher tide levels due to Lee's surge effects which created poor to no drainage of area coastal rivers, bays and sounds on during astronomical high tide cycles from 3-5 September (late night hours each day).

Began near Mon Louis (30.4527, -88.1098).

Other tornadoes from the same storm system

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

Source: NOAA Storm Events Database, event 347147. Narratives are written by the National Weather Service forecast office that issued the report.

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