Weather Alert in Georgia
Special Weather Statement issued July 1 at 4:55PM EDT by NWS Peachtree City GA
AREAS AFFECTED: Newton; Butts; Jasper
DESCRIPTION: At 455 PM EDT, a strong thunderstorm was over Rocky Plains, or 9 miles southwest of Covington, moving east at 15 mph. HAZARD...Up to 40 mph wind, frequent cloud to ground lightning and heavy rain. SOURCE...Radar indicated. IMPACT...Expect minor damage to tree limbs and blowing around of light, unsecured objects. Heavy rain may cause temporary street flooding especially in poor drainage areas. Locations impacted include... Covington, Porterdale, Newborn, Mansfield, Stewart, Worthville, Starrsville, Brick Store, Calvin, Eudora, North Alcovy, Fincherville, Oak Hill, Rocky Plains, and Magnet.
INSTRUCTION: People outdoors should seek shelter immediately. If you can hear thunder, you are close enough to be struck by lightning. Motorists should slow down and be prepared for possible loss of control due to hydroplaning.
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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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