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2011 Hackleburg–Phil Campbell tornado

2011 EF5 tornado in Alabama, U.S

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April 27th 2011 Tornado Franklin County, AL
Dstnmrgn · CC BY-SA 4.0

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The tornado first touched down at 3:05 p.m. CDT (2005 UTC) southwest of Hamilton, Alabama, before quickly becoming violent and reaching EF5 intensity as it approached and struck Hackleburg, destroying a large portion of the town. The tornado maintained EF5 intensity as it struck Phil Campbell, again sweeping numerous homes off foundations, and then peaking in intensity and width shortly afterwards as it entered more rural areas. It weakened somewhat thereafter but re-strengthened as it hit Tanner (previously hit by two F5 tornadoes in the 1974 Super Outbreak). It weakened after hitting Tanner and lifted just south of the Alabama–Tennessee border at 4:50 p.m. CDT (2150 UTC). In total, the tornado was on the ground for nearly two hours, making it the second-longest lived tornado of the outbreak. Hundreds of homes were either destroyed or reduced to foundations as a result of the tornado.

In total, the tornado killed 71 people across five counties. It was the deadliest single tornado ever to strike the state of Alabama as well as the deadliest in the United States since a 1955 tornado in Udall, Kansas killed 80 people – the Joplin EF5 tornado a month later killed 158. The path of the tornado was 102 miles (164 km) long and extended across much of Northern Alabama. Damage wrought by the tornado amounted to $1.29 billion (2011 USD), making it the seventh-costliest tornado in United States history, unaccounted for inflation.

Meteorological synopsis

Setup

The environmental conditions leading up to the 2011 Super Outbreak were among the "most conducive to violent tornadoes ever documented". On April 25, a vigorous upper-level shortwave trough moved into the Southern Plains states. Ample instability, low-level moisture, and wind shear all fueled a significant tornado outbreak from Texas to Tennessee; at least 64 tornadoes touched down on this day. An area of low pressure consolidated over Texas on April 26 and traveled east while the aforementioned shortwave trough traversed the Mississippi and Ohio River valleys. Another 50 tornadoes touched down on this day. The multi-day outbreak culminated on April 27 with the most violent day of tornadic activity since the 1974 Super Outbreak. Multiple episodes of tornadic activity ensued with two waves of mesoscale convective systems in the morning followed by a widespread outbreak of supercells from Mississippi to North Carolina during the afternoon into the evening.

Tornadic activity on April 27 was precipitated by a 995 mbar (hPa; 29.39 inHg) surface low situated over Kentucky and a deep, negatively tilted (aligned northwest to southeast) trough over Arkansas and Louisiana. A strong southwesterly surface jet intersected these systems at a 60° angle, an ageostrophic flow that led to storm-relative helicity values in excess of 500 m2s−2—indicative of extreme wind shear and a very high potential for rotating updrafts within supercells. Ample moisture from the Gulf of Mexico was brought north across the Deep South, leading to daytime high temperatures of 77 to 81 °F (25 to 27 °C) and dewpoints of 66 to 72 °F (19 to 22 °C). Furthermore, convective available potential energy (CAPE) values reached 2,500–3,000 J/kg.

Forecast

On the morning of April 27, a strong cold front with several areas of embedded low pressure extended from the Texas Hill Country northeastward towards the Arklatex and the Ozarks, and later into the lower Ohio Valley. Warm moist air was in place due to strong southerly flow ahead of the front over Mississippi, Alabama, and Tennessee. An upper level disturbance sparked a broad area of showers and thunderstorms as it moved across the frontal boundary on the previous evening. The eastern edge of the line of showers and storms continued to move eastward, in concert with the upper disturbance, reaching the northwest Alabama border around 2:00 a.m. CDT.

This produced the last and most violent round of severe weather, which began around 2:30 p.m. CDT for northern Alabama as supercells began to line up to the southwest of the area. During the early afternoon, the potential for destructive tornadoes was highlighted by the Storm Prediction Center's upgrade to a high risk for severe weather around 1:00 p.m. CDT. This prompted a particularly dangerous situation (PDS) tornado watch, which was issued for northern Alabama and portions of southern Tennessee at 1:45 p.m. CDT. The bulletin that accompanied the watch read:

THE NWS STORM PREDICTION CENTER HAS ISSUED A TORNADO WATCH FOR PORTIONS OF: MUCH OF ALABAMA, NORTHWEST GEORGIA, SOUTHEAST MISSISSIPPI, SOUTHERN MIDDLE TENNESSEE, EFFECTIVE THIS WEDNESDAY AFTERNOON AND EVENING FROM 145 PM UNTIL 1000 PM CDT.

...THIS IS A PARTICULARLY DANGEROUS SITUATION...

DESTRUCTIVE TORNADOES...LARGE HAIL TO 4 INCHES IN DIAMETER. THUNDERSTORM WIND GUSTS TO 80 MPH...AND DANGEROUS LIGHTNING ARE POSSIBLE IN THESE AREAS.

The potential for tornadoes ramped up from noon through 9:00 p.m. CDT. During this period, much of Mississippi and Alabama experienced numerous supercell thunderstorms that produced violent tornadoes, including four EF5 tornadoes, one being the Hackleburg tornado.

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