Weather Alert in North Carolina
High Wind Watch issued February 5 at 8:57PM EST until February 7 at 7:00PM EST by NWS Greenville-Spartanburg SC
AREAS AFFECTED: Avery; Alexander; Yancey; Mitchell; Buncombe; Southern Jackson; Transylvania; Henderson; Caldwell Mountains; Greater Caldwell; Burke Mountains; Greater Burke; McDowell Mountains; Eastern McDowell; Rutherford Mountains; Greater Rutherford; Polk Mountains; Eastern Polk; Greenville Mountains
DESCRIPTION: * WHAT...Northwest winds 20 to 30 mph with gusts up to 65 mph possible. * WHERE...Portions of western North Carolina and Upstate South Carolina. * WHEN...From Friday evening through Saturday evening. * IMPACTS...Damaging winds could blow down trees and power lines. Widespread power outages are possible. Travel could be difficult, especially for high profile vehicles. * ADDITIONAL DETAILS...The strong winds will result in cold wind chills across the mountains early Saturday morning, and some blowing snow near the Tennessee border.
INSTRUCTION: Be prepared for possible power outages. Take time now to fasten or shelter loose objects in a safe location prior to the onset of high winds. Stay tuned to NOAA Weather Radio or your favorite source of weather information for the latest updates. Additional details can be found at www.weather.gov/gsp.
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Weather Topic: What are Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
Next Topic: Sleet
Weather Topic: What is Snow?
Home - Education - Precipitation - Snow
Next Topic: Stratocumulus Clouds
Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake,
has unique characteristics, but all of them grow in a hexagonal structure.
Snowfall can last for sustained periods of time and result in significant buildup
of snow on the ground.
On the earth's surface, snow starts out light and powdery, but as it begins to melt
it tends to become more granular, producing small bits of ice which have the consistency of
sand. After several cycles of melting and freezing, snow can become very dense
and ice-like, commonly known as snow pack.
Next Topic: Stratocumulus Clouds
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