Weather Alert in North Carolina
Special Weather Statement issued February 5 at 7:05PM EST by NWS Wilmington NC
AREAS AFFECTED: Robeson; Bladen; Columbus; Inland Pender; Coastal Pender; Inland New Hanover; Coastal New Hanover; Inland Brunswick; Coastal Brunswick; Marlboro; Darlington; Dillon; Florence; Marion; Williamsburg; Coastal Horry; Inland Georgetown; Coastal Georgetown; Central Horry; Northern Horry
DESCRIPTION: Standing water from the recent rainfall and any leftover melting snow will result in patchy black ice along or across area roadways and thoroughfares as temperatures drop to and below 32 later this evening, and into the 20s overnight. Icy spots could form on paved surfaces such as bridges and overpasses, primary and especially less traveled secondary roads, parking lots, sidewalks and driveways. Black ice is difficult to see and distinguish from dry surfaces. The deceptive nature of black ice can catch you unaware while you are driving or walking, causing you to lose control of your motor vehicle or for one to slip and fall.
INSTRUCTION: If you plan to drive or walk, remain alert for those slick spots. Slow your driving speed and use care when walking on sidewalks, driveways or across parking lots. Slips and falls constitute a leading cause of injuries during the winter weather season.
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Weather Topic: What is Condensation?
Home - Education - Precipitation - Condensation
Next Topic: Contrails
Condensation is the process which creates clouds, and therefore
it is a crucial process in the water cycle.
Condensation is the change of matter from a state of gas into a state of liquid,
and it happens because water molecules release heat into the atmosphere and
become organized into a more closely packed structure, what we might see as
water droplets.
Water is always present in the air around us as a vapor, but it's too small for
us to see. When water undergoes the process of condensation it becomes organized
into visible water droplets. You've probably seen condensation happen before on the
surface of a cold drink!
Next Topic: Contrails
Weather Topic: What are Cumulonimbus Clouds?
Home - Education - Cloud Types - Cumulonimbus Clouds
Next Topic: Cumulus Clouds
The final form taken by a growing cumulus cloud is the
cumulonimbus cloud, which is very tall and dense.
The tower of a cumulonimbus cloud can soar 23 km into the atmosphere, although
most commonly they stop growing at an altitude of 6 km.
Even small cumulonimbus clouds appear very large in comparison to other cloud types.
They can signal the approach of stormy weather, such as thunderstorms or blizzards.
Next Topic: Cumulus Clouds
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