Weather Alert in Georgia
Flood Advisory issued August 2 at 5:07PM EDT until August 2 at 6:00PM EDT by NWS Charleston SC
AREAS AFFECTED: Evans, GA; Liberty, GA; Long, GA; McIntosh, GA; Tattnall, GA
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall continues. * WHERE...A portion of southeast Georgia, including the following counties, Evans, Liberty, Long, McIntosh and Tattnall. * WHEN...Until 600 PM EDT. * IMPACTS...Minor flooding in low-lying and poor drainage areas. * ADDITIONAL DETAILS... - At 506 PM EDT, Doppler radar indicated showers and thunderstorms with torrential rainfall extending from Mendes and Glennville east to Halfmoon Landing. Although the heaviest rains are pushing north of the area, the risk for minor flooding of low-lying and poor drainage areas continues. - Some locations that will experience flooding include... Hinesville, Reidsville, Glennville, Claxton, Darien, Ludowici, Fort Stewart, Tibet, Jones and McIntosh.
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles.
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Weather Topic: What are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
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