Weather Alert in Georgia
Special Weather Statement issued February 23 at 10:07AM EST by NWS Charleston SC
AREAS AFFECTED: Jenkins; Screven; Candler; Bulloch; Effingham; Tattnall; Evans; Inland Bryan; Coastal Bryan; Inland Chatham; Coastal Chatham; Long; Inland Liberty; Coastal Liberty; Inland McIntosh; Coastal McIntosh; Allendale; Hampton; Inland Colleton; Dorchester; Inland Berkeley; Inland Jasper; Beaufort; Coastal Colleton; Charleston; Coastal Jasper; Tidal Berkeley
DESCRIPTION: Breezy northwesterly winds will persist across southeast Georgia and southeast South Carolina today. Wind gusts around 25 mph and relative humidity values between 25 to 30 percent will be common across the area from late morning until sunset. These weather conditions will result in an increased wildfire risk today.
INSTRUCTION: Please refer to your local burn permitting authorities on whether you can burn. If you do, you are advised to use extreme caution.
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Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
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
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