Weather Alert in North Carolina
Winter Weather Advisory issued February 5 at 9:05PM EST until February 7 at 7:00AM EST by NWS Greenville-Spartanburg SC
AREAS AFFECTED: Madison; Yancey; Mitchell
DESCRIPTION: * WHAT...Snow expected above 3500 feet. Total snow accumulations between 1 and 3 inches with some locations up to 6 inches along the Tennessee border. Winds gusting as high as 65 mph. * WHERE...Madison, Mitchell, and Yancey Counties. * WHEN...From 1 PM Friday to 7 AM EST Saturday. * IMPACTS...The heavy snow will create snow covered roads and produce scattered power outages. The hazardous conditions could impact the Friday evening commute. Very strong winds could cause extensive damage to trees and power lines. * ADDITIONAL DETAILS...The frequent and strong wind gusts will result in some blowing and drifting of snow.
INSTRUCTION: 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 is Precipitation?
Home - Education - Precipitation - Precipitation
Next Topic: Rain
Precipitation can refer to many different forms of water that
may fall from clouds. Precipitation occurs after a cloud has become saturated to
the point where its water particles are more dense than the air below the cloud.
In most cases, precipitation will reach the ground, but it is not uncommon for
precipitation to evaporate before it reaches the earth's surface.
When precipitation evaporates before it contacts the ground it is called Virga.
Graupel, hail, sleet, rain, drizzle, and snow are forms of precipitation, but fog
and mist are not considered precipitation because the water vapor which
constitutes them isn't dense enough to fall to the ground.
Next Topic: Rain
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
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