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 Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
Weather Topic: What is Graupel?
Home - Education - Precipitation - Graupel
Next Topic: Hail
Graupel is a form of precipitation that is created by atmospheric conditions
which cause supercooled water droplets to contact snow crystals and freeze to
their surface.
Sometimes known as soft hail or snow pellets, graupel is delicate and easily
destroyed by touch. Whereas hail usually falls during severe weather, graupel
doesn't require such conditions to form, and can form in mild precipitation
similar to situations which produce snowfall.
Next Topic: Hail
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