Weather Alert in Georgia
Flood Watch issued August 2 at 3:12PM EDT until August 3 at 4:00AM EDT by NWS Tallahassee FL
AREAS AFFECTED: Quitman; Clay; Randolph; Calhoun; Terrell; Dougherty; Lee; Worth; Turner; Tift; Ben Hill; Irwin; Early; Miller; Baker; Mitchell; Colquitt; Cook; Berrien; Decatur; Grady; Thomas; Brooks; Lowndes; Lanier
DESCRIPTION: * WHAT...Flash flooding caused by excessive rainfall is possible across Southwest and South Central Georgia. * WHERE...For the following counties in South Central Georgia, Ben Hill, Berrien, Brooks, Colquitt, Cook, Irwin, Lanier, Lowndes, Thomas, Tift, Turner and Worth. In southwest Georgia, Baker, Calhoun, Clay, Decatur, Dougherty, Early, Grady, Lee, Miller, Mitchell, Quitman, Randolph and Terrell. * WHEN...Through 4 AM EDT Sunday Morning. * IMPACTS...Excessive runoff may result in flash flooding of roadways as well as greater impacts in urban areas where flood-prone neighborhoods could be especially vulnerable to rising water. Small creeks may also rise rapidly, leading to flooding. * ADDITIONAL DETAILS... - A very moist airmass is in place across the region and numerous showers and thunderstorms are expected to develop later this afternoon and evening across South Georgia. Due to the slow motion of these storms, some areas could see rainfall totals of 3 to 5 inches with isolated maximum amounts of 7 inches through tonight. - 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 flash flooding develop.
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Weather Topic: What is Condensation?
Home - Education - Precipitation - Condensation
Next Topic: Contrails
Condensation is the process which creates clouds, and therefore
it is a crucial process in the water cycle.
Condensation is the change of matter from a state of gas into a state of liquid,
and it happens because water molecules release heat into the atmosphere and
become organized into a more closely packed structure, what we might see as
water droplets.
Water is always present in the air around us as a vapor, but it's too small for
us to see. When water undergoes the process of condensation it becomes organized
into visible water droplets. You've probably seen condensation happen before on the
surface of a cold drink!
Next Topic: Contrails
Weather Topic: What are Cumulonimbus Clouds?
Home - Education - Cloud Types - Cumulonimbus Clouds
Next Topic: Cumulus Clouds
The final form taken by a growing cumulus cloud is the
cumulonimbus cloud, which is very tall and dense.
The tower of a cumulonimbus cloud can soar 23 km into the atmosphere, although
most commonly they stop growing at an altitude of 6 km.
Even small cumulonimbus clouds appear very large in comparison to other cloud types.
They can signal the approach of stormy weather, such as thunderstorms or blizzards.
Next Topic: Cumulus Clouds
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