Weather Alert in Georgia
Flood Warning issued August 2 at 6:43PM EDT until August 2 at 8:15PM EDT by NWS Charleston SC
AREAS AFFECTED: Chatham, GA
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall is expected. * WHERE...A portion of southeast Georgia, including the following county, Chatham. * WHEN...Until 815 PM EDT. * IMPACTS...Expect many areas of slow moving or standing water. * ADDITIONAL DETAILS... - At 641 PM EDT, Doppler radar indicated only light rain falling over central Chatham County. While no additional flash flooding is expected, many areas remain flooded around the Windsor Forest, Hunter Army Airfield and Downtown Savannah areas. It will take a bit longer for flood waters to recede. Remember, never drive into flooded areas! - Some locations that will experience flooding include... Windsor Forest, Hunter Army Airfield, Coffee Bluff, Midtown Savannah, Downtown Savannah, Montgomery, Garden City, Thunderbolt and Vernonburg. - This includes the following highways... I-16 near mile marker 162. I-95 in Georgia between mile markers 96 and 97. I-516 between mile markers 3 and 4.
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles.
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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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