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Overview

The most widespread severe thunderstorm activity in many months broke out across eastern Kentucky on Tuesday, May 16th. A warm front lifted to near the Mountain Parkway during the morning hours, ushering in a muggy airmass for those locations to the south of the Parkway. Sun shining on this juicy air mass helped build up moderate amounts of instability south of the warm front as temperatures warmed into the upper 70s to mid 80s there. Meanwhile, persistent cloud cover and a weak northeasterly breeze kept temperatures cooler and conditions much more stable north of the front.

Scattered showers and storms were observed near and north of the warm front earlier in the day, but a majority of the activity did not arrive until afternoon when a wave of low pressure rode directly along the stalled boundary. This low acted as a trigger for lift while also increasing the wind shear sufficiently to favor rotating supercell thunderstorms across most of eastern Kentucky. Several of the thunderstorms, especially near the Mountain Parkway southward to US-421, exhibited classic supercell structure and strong rotation. Within this corridor, multiple swaths of hail greater than 1 inch in diameter were observed. Additionally, the greatest turning of the winds in the low-levels (typically needed for the formation of tornadoes) occurred right along and south of the warm front (which was situated near the Mountain Parkway). It was within this zone that a storm moving along/near the warm front dropped a brief EF-1 tornado in the vicinity of the Hendricks and Foraker communities of Magoffin County moments past 4:45 PM. In the hour and 45 minutes preceding the tornado, a number of residents upstream of the tornado reportedly observed a funnel cloud along the Estill/Powell County line. However, an all-day search from a NWS Jackson Storm Survey Team turned up no tornado damage (though much of that area is remote forest land inaccessible from roadways). Further east in Pike County, another supercell moving along this same boundary pummeled the Kimper area with hail up to the size of tennis balls. A few dozen miles south of the boundary, another storm which organized over Leslie County dropped hail up to golf-ball size near Hazard. Further south from the warm front, storms tended to be less supercellular and instead generated strong outflows leading to bowing storm lines which produced damaging wind gusts.

Image
Rotating Supercell Passing near Powell/Estill County Line as Seen from West Irvine (Courtesy of Johnny Ray Feltner)
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