Weather Alert in North Carolina
Special Weather Statement issued February 5 at 8:16PM EST by NWS Newport/Morehead City NC
AREAS AFFECTED: Beaufort; Mainland Hyde; Jones; Pamlico; Northern Craven; Southern Craven; West Carteret; East Carteret; Inland Onslow; Coastal Onslow
DESCRIPTION: The mix of rain, snow, sleet, and ice pellets, has further dampened the ground near the Crystal Coast this evening resulting in fairly widespread wet spots across portions of Onslow to Carteret County and areas north to Beaufort and mainland Hyde Counties. With temps quickly forecast to fall below freezing tonight, don't think these more widespread wet spots will dry in time, so black ice has become a concern. This threat will last until about 9AM before temps quickly warm above freezing and the black ice threat greatly lowers. Biggest areas of concern will be across bridges, overpasses, and any elevated roadways. Thin sheets of ice, called black ice, may be difficult to see, especially during the pre-dawn hours. They may appear to be wet spots on the road. Motorists will have a difficult time determining which spots are just wet and which are icy. Motorists are advised to use extra caution. Allow ample distance between yourself and other vehicles, to avoid the risk of a collision if slippery conditions are encountered. Allow a little extra time to reach your destination safely.
INSTRUCTION: N/A
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Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
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