Weather Alert in Georgia
Severe Thunderstorm Warning issued May 2 at 9:28PM EDT until May 2 at 10:15PM EDT by NWS Peachtree City GA
AREAS AFFECTED: Hall, GA; Lumpkin, GA; White, GA
DESCRIPTION: SVRFFC The National Weather Service in Peachtree City has issued a * Severe Thunderstorm Warning for... Southeastern Lumpkin County in north central Georgia... White County in northeastern Georgia... Northeastern Hall County in north central Georgia... * Until 1015 PM EDT. * At 927 PM EDT, a severe thunderstorm was located near Sautee, or near Cleveland, moving northeast at 15 mph. HAZARD...60 mph wind gusts and penny size hail. SOURCE...Radar indicated. IMPACT...Expect damage to roofs, siding, and trees. * Locations impacted include... Cleveland, Clermont, Helen, Unicoi State Park, Robertstown, Mossy Creek, Anna Ruby Falls, Garland, Leaf, Smithgall Woods Conservation Are, Sautee, Qualatchee Lake, and Batesville.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building. If you see wind damage...hail or flooding...wait until the storm has passed...and then call the National Weather Service toll free at 1 8 6 6 7 6 3 4 4 6 6 or tweet us your report at NWSATLANTA.
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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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