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 is Evaporation?
Home - Education - Precipitation - Evaporation
Next Topic: Fog
Evaporation is the process which returns water from the earth
back to the atmosphere, and is another crucial process in the water cycle.
Evaporation is the transformation of liquid into gas, and it happens because
molecules are excited by the application of energy and turn into vapor.
In order for water to evaporate it has to be on the surface of a body of water.
Next Topic: Fog
Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
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