Weather Alert in North Carolina
Special Weather Statement issued February 4 at 10:34PM EST by NWS Greenville-Spartanburg SC
AREAS AFFECTED: Avery; Alexander; Iredell; Davie; Madison; Yancey; Mitchell; Haywood; Buncombe; Catawba; Rowan; Transylvania; Henderson; 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; Cherokee; York; Pickens Mountains; Greenville Mountains; Central Greenville; Northern Spartanburg; Southern Spartanburg
DESCRIPTION: Snow showers are developing along the Escarpment and are expected to generally drift east into the Piedmont from late evening through the overnight. Snow showers are possible roughly along a line from Greenville to Spartanburg to York and areas north and east. Most locations should only see a trace on mainly grassy and elevated surface. But localized accumulations of up to an inch are possible in the heavier showers. There is also still melting snow from last weekend's storm across portions of the North Carolina Foothills and Piedmont that may refreeze by daybreak Thursday and produce black ice. Be prepared for slick spots, especially on bridges and overpasses and any untreated roadways. Use extra caution when walking on sidewalks, driveways, and in parking lots.
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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