Weather Alert in North Carolina
High Wind Warning issued February 6 at 1:08PM EST until February 7 at 7:00PM EST by NWS Greenville-Spartanburg SC
AREAS AFFECTED: Buncombe; Southern Jackson; Transylvania; Henderson; Caldwell Mountains; Burke Mountains; McDowell Mountains; Rutherford Mountains; Polk Mountains
DESCRIPTION: * WHAT...Northwest winds 20 to 30 mph with gusts up to 65 mph expected. * WHERE...Buncombe, Burke Mountains, Caldwell Mountains, Henderson, McDowell Mountains, Polk Mountains, Rutherford Mountains, Southern Jackson, and Transylvania Counties. * WHEN...From 7 PM this evening to 7 PM EST Saturday. * IMPACTS...Damaging winds will blow down trees and power lines. Widespread power outages are expected. Travel will be difficult, especially for high profile vehicles.
INSTRUCTION: Avoid being outside near trees. If caught outside, watch for falling debris or tree limbs. Remain in the lower levels of your home during the windstorm and avoid windows and overhanging trees. Use caution if you must drive. Stay tuned to NOAA Weather Radio or your favorite source of weather information for the latest updates. Additional details can be found at www.weather.gov/gsp.
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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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