Weather Alert in Georgia
Special Weather Statement issued February 8 at 12:56AM EST by NWS Greenville-Spartanburg SC
AREAS AFFECTED: Rabun; Habersham; Stephens; Franklin; Hart; Elbert
DESCRIPTION: Dead brush and leaf litter have become very dry in northeast Georgia, and will continue to dry today as relative humidity becomes very low, falling to less than 25 percent. Winds will be light, but the low humidity and fuel moisture together mean that fires will be able to spread quickly once started. Please refer to your local burn permitting authorities on whether you can burn today. If you do burn, use extreme caution since fires can quickly get out of hand under these conditions.
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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