Weather Alert in Georgia
Severe Thunderstorm Warning issued July 14 at 4:39PM EDT until July 14 at 5:45PM EDT by NWS Charleston SC
AREAS AFFECTED: Bryan, GA; Bulloch, GA; Effingham, GA
DESCRIPTION: SVRCHS The National Weather Service in Charleston has issued a * Severe Thunderstorm Warning for portions of... Bryan County in southeastern Georgia... Bulloch County in southeastern Georgia... Effingham County in southeastern Georgia... * Until 545 PM EDT. * At 439 PM EDT, a severe thunderstorm was located near Stilson, moving south at 20 mph. HAZARD...60 mph wind gusts and small hail. SOURCE...Radar indicated. IMPACT...Expect damage to roofs, siding, and trees. * Locations impacted include... Springfield, Pembroke, Lanier, Rincon, Guyton, Pineora, Marlow, Blitchton, Stilson and Bay. This includes I-16 between mile markers 131 and 147.
INSTRUCTION: Seek shelter inside a well-built structure and stay away from windows. This storm is capable of producing damaging winds. Continuous cloud to ground lightning is occurring with this storm. Lightning is one of nature's leading killers. Remember, if you can hear thunder, you are close enough to be struck by lightning.
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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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