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2014 Mayflower–Vilonia tornado

2014 EF4 tornado in central Arkansas, U.S.

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Dash cam capture of the violent EF4 tornado that devastated Vilonia, Arkansas on April 27, 2014
Ian Gates - Dash Cam (No human input was involved) · Public domain

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The tornado touched down near the western edge of Pulaski County, moving to the northwest before impacting Paron at EF3 intensity, killing three people and damaging several residential buildings as it moved by. The tornado continued to move to the northwest as it left the community in ruins, reaching EF4 intensity for the first time as it entered the city limits of Mayflower. The tornado produced heavy structural damage as it tore through the southern edge of the town, killing three people. The tornado later hit Vilonia, where it produced high-end EF4 damage. The tornado dissipated a short time later.

On April 29, Faulkner County was declared a federal disaster area by President Barack Obama, who was visiting the town of Vilonia to survey the damage and speak with families of the victims. The declaration allowed residents to receive federal aid and low-cost loans to cover uninsured losses. The final rating of the tornado was a source of controversy, with some damage analysts concluding that EF5 damage was plausible.

Meteorological synopsis

Setup

The Storm Prediction Center (SPC) indicated the potential for a large-scale tornado outbreak for six days in advance on its 4–8 day outlook, beginning early on April 19 valid at day 5. While models diverged on the exact nature and intensity of the expected mid-level shortwave trough, there was broad support for a dry line to develop in central Oklahoma. By April 22, the SPC expanded the threat zone for day 6 for the remainder of Oklahoma and central High Plains region, with strong upper-level winds to spread over the central High Plains. Three days later, a Day 3 moderate risk was issued early on April 25 for the Ark-La-Tex region, citing the increased risk for a severe weather outbreak, with the risk of trailing supercells.

Forecast

The strong mid-level shortwave trough developed into a closed low-pressure area as the system occluded over the central High Plains on April 27, 2014. An associated surface cyclone reached peak intensity while a trailing cold front moved eastward across eastern Kansas, eastern Oklahoma and northern Texas. There were two areas where severe weather was expected: morning prefrontal convection from Kansas and Oklahoma into Missouri and Iowa and warm sector supercell development across southeast Oklahoma and northeast Texas into Arkansas. By 20:00 UTC on April 27, the SPC issued a rare high risk for much of central Arkansas and a 30% hatched risk for tornadoes across the same corridor, citing the anticipation of numerous supercells capable of producing intense tornadoes. Expected thermodynamic conditions of storm-relative helicity values in of 300–400 m2s−2, convective available potential energy (CAPE) values of 2,500–3,000 J/kg−1, a 40–50 kn low level jet and boundary-layer dewpoints of 57 to 61 °F (14 to 16 °C) were expected to foster supercell development and strong to intense tornadoes across Arkansas, along with very large hail. A particularly dangerous situation (PDS) tornado watch was issued at that time for central Arkansas, where the Mayflower–Vilonia tornado would soon develop.

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