Weather Alert in Georgia
Flood Warning issued August 20 at 10:49PM EDT by NWS Peachtree City GA
AREAS AFFECTED: Fulton, GA
DESCRIPTION: ...The National Weather Service in Peachtree City GA has issued a Flood Warning for the following rivers in Georgia... Proctor Creek at Jackson Parkway at Atlanta affecting Fulton County. * WHAT...Minor flooding is occurring. * WHERE...Proctor Creek at Jackson Parkway at Atlanta. * WHEN...From this evening until further notice. * IMPACTS...At 13 feet, Flood stage is reached. Minor flooding begins in the woodlands along the creek upstream and downstream from the gage on Jackson Parkway. This includes low lying areas of a pet cemetery just downstream from the bridge on the left bank. * ADDITIONAL DETAILS... - At 10:30 PM EDT Wednesday the stage was 13.5 feet and rising. - Forecast...No forecast is available for this location. - Flood stage is 13 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Be especially cautious at night when it is harder to recognize the dangers of flooding. Additional information is available at weather.gov/atlanta.
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Weather Topic: What is Precipitation?
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Precipitation can refer to many different forms of water that
may fall from clouds. Precipitation occurs after a cloud has become saturated to
the point where its water particles are more dense than the air below the cloud.
In most cases, precipitation will reach the ground, but it is not uncommon for
precipitation to evaporate before it reaches the earth's surface.
When precipitation evaporates before it contacts the ground it is called Virga.
Graupel, hail, sleet, rain, drizzle, and snow are forms of precipitation, but fog
and mist are not considered precipitation because the water vapor which
constitutes them isn't dense enough to fall to the ground.
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Weather Topic: What are Shelf Clouds?
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A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
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