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 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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