Weather Alert in North Carolina
Winter Weather Advisory issued February 21 at 9:49PM EST until February 24 at 12:00AM EST by NWS Greenville-Spartanburg SC
AREAS AFFECTED: Swain
DESCRIPTION: * WHAT...Snow expected above 3500 feet. Total snow accumulations mainly between 3 and 7 inches, with a foot or more possible on the high peaks of the Smokies. Up to an inch is possible in the valleys beneath the Smokies. * WHERE...The high elevations of Swain County. * WHEN...From midnight tonight until midnight EST Monday Night. * IMPACTS...The heavy snow will make many roads impassable, mainly in the higher elevations. The hazardous conditions could impact the Monday morning and evening commutes. * ADDITIONAL DETAILS...Winds gusting from 35 to 45 mph could result in areas of blowing snow and very low visibility in the high elevations Sunday night and Monday.
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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