Weather Alert in North Carolina
Winter Weather Advisory issued February 22 at 1:24PM EST until February 24 at 12:00AM EST by NWS Greenville-Spartanburg SC
AREAS AFFECTED: Mitchell
DESCRIPTION: * WHAT...For the Winter Storm Warning above 3500 feet, heavy snow. Additional snow accumulations between 1 and 11 inches. Winds gusting as high as 60 mph. For the Winter Weather Advisory below 3500 feet, snow. Additional snow accumulations up to 6 inches. Winds gusting as high as 55 mph. Wind chills as cold as 5 degrees below 0 early Monday morning. * WHERE...Mitchell County. * WHEN...Until midnight EST Monday Night. * IMPACTS...Heavy will make many roads impassable. The weight of the snow on tree limbs and power lines could produce isolated outages. The hazardous conditions could impact the Monday morning and evening commutes. Strong winds could cause extensive damage to trees and power lines.
INSTRUCTION: Monitor the latest forecasts for updates on this situation. Slow down and use caution while traveling. If you must travel, keep an extra flashlight, food, and water in your vehicle in case of an emergency. Slow down and use caution while traveling. The latest road conditions for the state you are calling from can be obtained by calling 5 1 1.
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Weather Topic: What are Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
Next Topic: Sleet
Weather Topic: What is Snow?
Home - Education - Precipitation - Snow
Next Topic: Stratocumulus Clouds
Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake,
has unique characteristics, but all of them grow in a hexagonal structure.
Snowfall can last for sustained periods of time and result in significant buildup
of snow on the ground.
On the earth's surface, snow starts out light and powdery, but as it begins to melt
it tends to become more granular, producing small bits of ice which have the consistency of
sand. After several cycles of melting and freezing, snow can become very dense
and ice-like, commonly known as snow pack.
Next Topic: Stratocumulus Clouds
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