Weather Alert in North Carolina
Winter Weather Advisory issued February 5 at 9:05PM EST until February 7 at 7:00AM EST by NWS Greenville-Spartanburg SC
AREAS AFFECTED: Avery
DESCRIPTION: * WHAT...Snow expected. Total snow accumulations of 1 to 4 inches, with some locations up to 6 inches near the Tennessee border. Winds gusting as high as 65 mph. * WHERE...Avery County. * WHEN...From 1 PM Friday to 7 AM EST Saturday. * IMPACTS...The heavy snow will create snow covered roads and produce scattered power outages. The hazardous conditions could impact the Friday evening commute. Very strong winds could cause extensive damage to trees and power lines. * ADDITIONAL DETAILS...The frequent and strong wind gusts will result in some blowing and drifting of snow. Wind chill values will drop down to around minus 5 degrees early Saturday morning.
INSTRUCTION: Slow down and use caution while traveling. The latest road conditions for the state you are calling from can be obtained by calling 5 1 1.
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Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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