Weather Alert in Georgia
Flood Watch issued August 11 at 6:09AM EDT until August 11 at 6:00PM EDT by NWS Charleston SC
AREAS AFFECTED: Inland Bryan; Coastal Bryan; Inland Chatham; Coastal Chatham; Inland Liberty; Coastal Liberty; Inland McIntosh; Coastal McIntosh; Beaufort; Coastal Colleton; Charleston; Coastal Jasper
DESCRIPTION: * WHAT...Flash flooding caused by excessive rainfall continues to be possible. * WHERE...Portions of southeast Georgia, including the following areas, Coastal Bryan, Coastal Chatham, Coastal Liberty, Coastal McIntosh, Inland Bryan, Inland Chatham, Inland Liberty and Inland McIntosh and southeast South Carolina, including the following areas, Beaufort, Charleston, Coastal Colleton and Coastal Jasper. * WHEN...Until 6 PM EDT this evening. * IMPACTS...Excessive runoff may result in flooding of rivers, creeks, streams, and other low-lying and flood-prone locations. Flooding may occur in poor drainage and urban areas. Extensive street flooding and flooding of creeks and rivers are possible. * ADDITIONAL DETAILS... - Additional bands of showers and thunderstorms will impact the coast of Southeast South Carolina and Southeast Georgia today. Much of this area has observed significant rainfall over the past several days. With saturated soil conditions in place, it will not take too much additional heavy rainfall to produce urban flooding and flash flooding, especially in the more urbanized areas around Charleston, Beaufort, Savannah and Hinesville. Localized rainfall amounts in excess of 4 inches can be expected through late afternoon. - http://www.weather.gov/safety/flood
INSTRUCTION: Be prepared to protect life and property, especially in areas prone to flooding. If flooding develops, move to higher ground immediately. If driving, be prepared for flooded roadways and possible road closures.
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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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