Weather Alert in Missouri

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Flood Warning issued April 2 at 3:21PM CDT until April 4 at 5:17PM CDT by NWS Kansas City/Pleasant Hill MO

AREAS AFFECTED: Carroll, MO

DESCRIPTION: ...The Flood Warning is extended for the following rivers in Missouri... Wakenda Creek at Carrollton affecting Carroll County. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Wakenda Creek at Carrollton. * WHEN...Until Saturday afternoon. * IMPACTS...At 16.0 feet, Flooding of low-lying undeveloped areas along the creek begins. * ADDITIONAL DETAILS... - At 3:00 PM CDT Thursday the stage was 16.2 feet. - Forecast...The river is expected to rise to a crest of 16.7 feet tomorrow morning. It will then fall below flood stage tomorrow afternoon. - Flood stage is 16.0 feet. - http://www.weather.gov/safety/flood

INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. This product along with additional weather and stream information is available at www.weather.gov/kc/.

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Weather Topic: What is Condensation?

Home - Education - Precipitation - Condensation

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

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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