Weather Alert in North Carolina
Special Weather Statement issued February 28 at 10:07PM EST by NWS Wilmington NC
AREAS AFFECTED: Robeson; Marlboro; Darlington; Dillon; Florence; Marion; Williamsburg; Inland Georgetown; Coastal Georgetown
DESCRIPTION: Areas where low clouds persisted during Saturday afternoon will be the prime locations where areas of fog reducing visibility to 1 to 3 miles will develop. Within these areas, locally dense fog is likely that will further reduce visibility to near 0 at times resulting in hazardous driving conditions. The fog will persist into Sunday morning and should disperse by 9 or 10 am the latest.
INSTRUCTION: Motorists encountering the fog should immediately SLOW down, make use of their low beam headlights and allow extra distance between you and the vehicle ahead in case of a sudden stop.
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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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