Flash Flood in Roanoke (c) County, Virginia

Glade Creek was observed out of its banks and flowing across Walnut Avenue at least 6 inches deep due to between 3 and locally 5 inches of rainfall within a 2-hour period falling in the basin. Rainfall rates were observed to be as high as 5 inches per hour at times. No damage was reported to the road, and it was reopened to traffic after the flooding receded.

An upper level storm system crossed the region during peak heating. The passage of this system aided in the lift needed for thunderstorm development within an already very moist and unstable atmosphere. The environment spawned scattered severe thunderstorms which produced damaging winds. In addition, storms were at times slow-moving, with winds up to 700 mb averaging around 10 knots from the southwest. Surface-based CAPEs across central Virginia varied from 1,500 to over 2,000 J/Kg during late afternoon, while precipitable water values varied from 1.2 inches across the Mountain Empire to 1.6 inches across the Southside area of Virginia. The high instability and abundant atmospheric moisture combined to produce storms with high rainfall rates, at times observed to be up to 5 inches per hour.