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 is Drizzle?
Home - Education - Precipitation - Drizzle
Next Topic: Evaporation
Drizzle is precipitation in the form of water droplets which are
smaller than raindrops.
Drizzle is characterized by fine, gently falling droplets and typically does not
impact human habitation in a negative way. The exception to this is freezing drizzle,
a condition where drizzle freezes immediately upon reaching earth's surface.
Freezing drizzle is still less dangerous than freezing rain, but can
potentially result in hazardous road conditions.
Next Topic: Evaporation
Weather Topic: What is Fog?
Home - Education - Cloud Types - Fog
Next Topic: Fractus Clouds
Fog is technically a type of stratus cloud, which lies along the
ground and obscures visibility.
It is usually created when humidity in the air condenses into tiny water droplets.
Because of this, some places are more prone to foggy weather, such as regions
close to a body of water.
Fog is similar to mist; both are the appearance of water droplets suspended in
the air, but fog is the term applied to the condition when visibility is less than 1 km.
Next Topic: Fractus Clouds
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