Weather Alert in Georgia
Flood Watch issued August 22 at 9:43AM EDT until August 23 at 2:00AM EDT by NWS Tallahassee FL
AREAS AFFECTED: Dougherty; Lee; Worth; Turner; Tift; Ben Hill; Irwin; Cook; Berrien
DESCRIPTION: * WHAT...Flash flooding caused by excessive rainfall is possible. * WHERE...For the following counties in South Central Georgia, Ben Hill, Berrien, Cook, Dougherty, Irwin, Lee, Tift, Turner and Worth. * WHEN...From 5 PM EDT this afternoon through late tonight. * IMPACTS...Runoff from heavy rainfall may result in flooding of roads, creeks and streams as well as impacting other low-lying and flood-prone locations. * ADDITIONAL DETAILS... - A very moist environment is in place across the region. Late afternoon and early evening thunderstorms are expected to develop and produce locally heavy rainfall across the watch area. Rainfall amounts of 3 to 5 inches are expected with isolated heavier totals to near 7 inches. These amounts could cause flash flooding. - http://www.weather.gov/safety/flood
INSTRUCTION: You should monitor later forecasts and be alert for possible Flash Flood Warnings. Those living in areas prone to flooding should be prepared to take action should flooding develop.
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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
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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