Weather Alert in North Carolina
Special Weather Statement issued February 26 at 10:35PM EST by NWS Greenville-Spartanburg SC
AREAS AFFECTED: Alexander; Iredell; Davie; Catawba; Rowan; Cleveland; Lincoln; Gaston; Mecklenburg; Cabarrus; Union; Caldwell Mountains; Greater Caldwell; Burke Mountains; Greater Burke; McDowell Mountains; Eastern McDowell; Rutherford Mountains; Greater Rutherford; Polk Mountains; Eastern Polk
DESCRIPTION: Patchy dense fog has formed across portions of the Piedmont of the Carolinas, particularly near bodies of water, where visibility is less than a half mile in spots. The remainder of the night generally will be foggy, with dense fog and very low visibility becoming increasingly common after midnight. Visibility may decrease suddenly and over short distances due to the patchy nature of the fog. Motorists traveling on area roadways should use extra caution. Slow down, increase following distance, and turn on your low-beam headlights.
INSTRUCTION: N/A
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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
Weather Topic: What are Cirrus Clouds?
Home - Education - Cloud Types - Cirrus Clouds
Next Topic: Condensation
Cirrus clouds are high-level clouds that occur above 20,000 feet
and are composed mainly of ice crystals.
They are thin and wispy in appearance.
What do they indicate?
They are often the first sign of an approaching storm.
Next Topic: Condensation
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