On the second day of a developing heat wave, under a sunny sky, afternoon temperatures reached above 100 degrees across most of northeast Kentucky. For example, Warnock in Greenup County had 104 degrees. Both Grayson and Ashland reached 103 degrees that Friday afternoon. Meanwhile, an area of multi-cellular convection had moved out of northern Illinois that morning. It continued to organize and strengthen, as it propagated east and southeast across northern Indiana into western Ohio during the afternoon. As it moved toward southeast Ohio, it had already formed into a large arch of storms, or bow, with a developing cool pool in its wake. The temperature contrast between the air ahead of the developing derecho, compared to that in its wake was reaching 30 to 35 degrees. The resultant wind shift in the cool pool resulted in strong moisture convergence on the leading edge of the complex. This in turn, helped drive the storms further southeast, away from the mid and upper level wind support. However, the complex was diving right into that hot air that had obtained large convective available potential energy, on the order of 4000 to 5000 j/kg.
The complex crossed the Ohio River into northeast Kentucky just after the hottest time of the day. The outflow, or gust front, had already outraced the rain. There were even brush fires ahead of the gust front. The wind with the gust front picked up dust and debris in some areas. The mature system caused the strong gusts to be longer in duration than found in most severe thunderstorms. In some cases the strong wind gusts lasted around 10 minutes.
Wind gusts of 55 to 70 mph were likely with the leading gust front across portions of northeast Kentucky. In the wake of these stronger winds gusts, the storms only provided around a third of an inch of rain or less. Warnock had around a third of an inch of rain, while Ashland measured only 0.14 inches. Grayson had a meager 0.08 inches.
The wind caused trees and large branches to fall in scattered locations. Roads were temporarily blocked. However, the largest impact was on the electric power grid. Prolong power outages occurred. The lack of electricity in the midst of the heat wave, disrupted the daily routines of many citizens for several days. On the order of 25 to 30 thousand customers were without electricity in these 4 northeast Kentucky counties. It took some 4 to 7 days to restored electricity in some areas. Workers trying to restore the electricity had to take frequent breaks due to the heat and the safety equipment they had to wear. Water and ice were in high demand. Refrigerated food spoiled.