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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North America Water Vapor (Moisture)
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Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
Weather Topic: What are Altostratus Clouds?
Home - Education - Cloud Types - Altostratus Clouds
Next Topic: Cirrocumulus Clouds
Altostratus clouds form at mid to high-level altitudes
(between 2 and 7 km) and are created by a warm, stable air mass which causes
water vapor
to condense as it rise through the atmosphere. Usually altostratus clouds are
featureless sheets characterized by a uniform color.
In some cases, wind punching through the cloud formation may give it a waved
appearance, called altostratus undulatus. Altostratus clouds
are commonly seen with other cloud formations accompanying them.
Next Topic: Cirrocumulus Clouds
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