Weather Alert in Alabama
Flash Flood Warning issued August 2 at 11:11PM CDT until August 3 at 2:15AM CDT by NWS Birmingham AL
AREAS AFFECTED: Calhoun, AL; Cleburne, AL
DESCRIPTION: FFWBMX The National Weather Service in Birmingham has issued a * Flash Flood Warning for... Northeastern Calhoun County in east central Alabama... Northeastern Cleburne County in east central Alabama... * Until 215 AM CDT. * At 1111 PM CDT, Doppler radar indicated thunderstorms producing heavy rain across the warned area. Between 2 and 3 inches of rain are estimated to have fallen across northern portions of Calhoun and Cleburne Counties. Flash flooding is ongoing or expected to begin shortly. HAZARD...Flash flooding caused by thunderstorms. SOURCE...Radar. IMPACT...Flash flooding of small creeks and streams, urban areas, highways, streets and underpasses as well as other poor drainage and low-lying areas. * Some locations that may experience flash flooding include... Jacksonville, Piedmont, Glencoe, Weaver, Fruithurst, Jacksonville State University, Mars Hills, Alexandria, Muscadine, Southside, Liberty Hill, Coleman Lake And Campground, Knightens Crossroads, Sweetwater Lake, Oak Level, Borden Springs, Sulphur Springs and Wellington.
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Be especially cautious at night when it is harder to recognize the dangers of flooding. Please report observed flooding to local emergency services or law enforcement and request they pass this information to the National Weather Service when you can do so safely.
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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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