Snow Across the Great Lakes, Central Appalachians, and Northeast; Unsettled Weather in the West

Light to moderate snow will continue into Saturday over the Great Lakes, Central Appalachians, and Northeast. This weekend into next week, a series of atmospheric rivers will bring gusty winds, periods of heavy rain, and mountain snow to northern California and the Pacific Northwest. Colder temperatures are in store for the weekend from the Great Lakes to East Coast. Read More >

Here in the Western Carolinas, we receive our fair share of thunderstorms. This is due to our proximity to the Gulf of Mexico and the Atlantic Ocean, which provide two sources of warm, humid air in the warm season. The mountains also play a role in our thunderstorm frequency, as air flowing around and up mountain slopes can provide the lift that is required to push the unstable air up into the atmosphere. On days when the atmosphere is particularly unstable, some thunderstorms may become severe.

Damaging wind gusts are the most common form of severe weather across the western Carolinas and northeast Georgia. Damaging wind gusts, often called “downbursts,” form in association with the downdraft. They are caused when sinking air within the downdraft accelerates toward the surface, then spreads horizontally away from the storm after impacting the ground.

Although most downbursts cause wind gusts of around 60 mph, speeds of 100 mph or more are possible. Wind gusts of this magnitude can cause extensive damage to trees, power lines, and manufactured homes. This is equivalent to the wind speeds produced by weak tornadoes. This is a very important point: downbursts can produce damage similar to a weak or even moderately strong tornado. The peak time of year for downbursts across the region is June

and July. They are especially common in the piedmont. A typical piedmont county experiences at least one event on four to seven days per year.

The second most common form of severe weather across the Carolinas and northeast Georgia is large hail. Hail is simply ice that develops in the upper levels of a tall thunderstorm, where temperatures are well below freezing. The strong updrafts

strong updrafts associated with such storms suspend ice particles aloft within the storm’s core. These suspended hailstones are subject to collisions with other ice particles. These collisions cause the hailstones to grow. Eventually, the hail will become too large and

heavy for the updraft to support. allowing the hail to fall to the ground via the downdraft. Large hailstones across the western Carolinas and northeast Georgia rarely exceed the size of a quarter. However, hail as large as softballs has been reported across the area as recently as 2011.

In this region, large hail is most common in the piedmont of the western Carolinas, where two to four days of large hail are observed in a given year. Hail that is the size of a golf ball or larger is quite rare, but is observed on about one day per year across the piedmont. The peak time of year for large hail is May and June.

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