Weather Alert in Georgia
Flood Watch issued August 22 at 8:57AM EDT until August 23 at 12:00AM EDT by NWS Jacksonville FL
AREAS AFFECTED: Coffee; Jeff Davis; Bacon; Appling; Wayne; Atkinson; Pierce; Brantley; Inland Glynn; Coastal Glynn; Inland Camden; Coastal Camden; Northern Ware; Northeastern Charlton
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall is possible. * WHERE...A portion of southeast Georgia, including the following areas, Appling, Atkinson, Bacon, Brantley, Coastal Camden, Coastal Glynn, Coffee, Inland Camden, Inland Glynn, Jeff Davis, Northeastern Charlton, Northern Ware, Pierce and Wayne. * WHEN...From 5 PM EDT this afternoon through this evening. * IMPACTS...Excessive runoff may result in flooding of rivers, creeks, streams, and other low-lying and flood-prone locations. Flooding may occur in poor drainage and urban areas. * ADDITIONAL DETAILS... - A frontal boundary positioned across southeastern Georgia will develop widespread thunderstorms and slow moving, heavy downpours late this afternoon through this evening. The risk for flooding and potential flash flooding will increase during this time frame, with locations in urban and normally flood prone areas being most at risk for substantial flooding. Rainfall amounts of 1-2 inches, with localized totals of 3-4 inches will be possible, with very heavy rainfall rates expected within heavier downpours. - http://www.weather.gov/safety/flood
INSTRUCTION: You should monitor later forecasts and be alert for possible 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 Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
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.
Next Topic: Sleet
Weather Topic: What is Snow?
Home - Education - Precipitation - Snow
Next Topic: Stratocumulus Clouds
Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake,
has unique characteristics, but all of them grow in a hexagonal structure.
Snowfall can last for sustained periods of time and result in significant buildup
of snow on the ground.
On the earth's surface, snow starts out light and powdery, but as it begins to melt
it tends to become more granular, producing small bits of ice which have the consistency of
sand. After several cycles of melting and freezing, snow can become very dense
and ice-like, commonly known as snow pack.
Next Topic: Stratocumulus Clouds
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