Freezing rain air at the surface within the region of high pressure. The warm air from the Gulf of Mexico is often the fuel for freezing precipitation. Freezing rain develops when falling snow encounters a layer of warm air aloft, typically around the 800 mbar (800 hPa) level, causing the snow to melt and become rain. As the rain continues to fall, it passes through a layer of subfreezing air just above the surface and cools to a temperature below freezing (). If this layer of subfreezing air is sufficiently deep, the raindrops may have time to freeze into ice pellets (sleet)
Wilkes County, North Carolina spring and summer months; and rain, snow, sleet, and freezing rain all occur at times during the winter, with the frequency increasing with the altitude. Severe weather is not common in Wilkes but does occur. Tornadoes are rare, but severe thunderstorms can bring strong winds which can down trees and power lines, as well as cause hail. In October 2017, a rare EF 1 tornado touched down in the towns of Wilkesboro and North Wilkesboro, and then moved through the Mulberry, Fairplains, and Hays communities, causing significant damage. Wilkes County is far enough inland that hurricanes rarely cause problems, but