Weather Alert in Georgia
Special Weather Statement issued March 29 at 4:05AM EDT by NWS Greenville-Spartanburg SC
AREAS AFFECTED: Rabun; Habersham; Stephens; Franklin; Hart; Elbert; Avery; Alexander; Iredell; Davie; Madison; Yancey; Mitchell; Swain; Haywood; Buncombe; Catawba; Rowan; Graham; Northern Jackson; Macon; Southern Jackson; Transylvania; Henderson; Cleveland; Lincoln; Gaston; Mecklenburg; Cabarrus; Union; Caldwell Mountains; Greater Caldwell; Burke Mountains; Greater Burke; McDowell Mountains; Eastern McDowell; Rutherford Mountains; Greater Rutherford; Polk Mountains; Eastern Polk; Cherokee; York; Anderson; Abbeville; Laurens; Union; Chester; Greenwood; Oconee Mountains; Pickens Mountains; Greenville Mountains; Greater Oconee; Greater Pickens; Central Greenville; Southern Greenville; Northern Spartanburg; Southern Spartanburg
DESCRIPTION: While moisture is expected to begin slowly recovering today, another very dry afternoon is expected with relative humidity values between 15 and 25 percent forecast across much of the area. Although winds will be mostly light, between 5 and 10 mph, the dry air combined with very dry vegetation will result in a continuation of elevated fire danger. Statewide burn bans are in effect for both North Carolina and South Carolina until further notice. Open burning of any kind is subject to fines until the bans are lifted.
INSTRUCTION: N/A
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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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