Weather Alert in Iowa
Flood Warning issued August 11 at 9:45AM CDT until August 14 at 9:00AM CDT by NWS Quad Cities IA IL
AREAS AFFECTED: Clinton, IA; Scott, IA
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Iowa... Wapsipinicon River near De Witt 4S affecting Scott and Clinton Counties. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Wapsipinicon River near De Witt 4S. * WHEN...Until late Thursday morning. * IMPACTS...At 11.0 feet, Flood Stage. Water affects County Road E63 north of the river near Toronto and affects the lowest roads in Buena Vista. * ADDITIONAL DETAILS... - At 9:30 AM CDT Monday the stage was 11.3 feet. - Forecast...The river is cresting and will fall below flood stage late this evening to 10.6 feet early Wednesday morning. It will then rise to flood stage early Thursday morning. It will fall for the remainder of the period. - Flood stage is 11.0 feet.
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. The next statement will be issued by Tuesday morning at 945 AM CDT.
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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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