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 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
Weather Topic: What are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
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