Weather Alert in Indiana

Recent Locations: Wabash, IN  

Flood Warning issued March 4 at 12:07PM EST until March 8 at 11:45AM EDT by NWS Indianapolis IN

AREAS AFFECTED: Bartholomew, IN; Jackson, IN

DESCRIPTION: ...The Flood Warning is extended for the following rivers in Indiana... Big Blue River at Shelbyville. East Fork White River at Seymour. Flatrock River near Columbus. East Fork White River at Columbus. .Rainfall amounts between two and four inches over parts of central and southern Indiana have led to rises and some flooding on area rivers. Additional rainfall of one to three inches this evening into Thursday morning, with locally higher amounts possible, will bring widespread minor river flooding with pockets of moderate flooding to much of the East Fork White and lower White River basins. * WHAT...Minor flooding is forecast. * WHERE...East Fork White River at Columbus. * WHEN...From this evening to late Sunday morning. * IMPACTS...At 12.5 feet, SR 11 north of CR 200 S flooded. This occurs about once every 1 to 2 years. * ADDITIONAL DETAILS... - At 11:00 AM EST Wednesday the stage was 6.0 feet. - Forecast...The river is expected to rise above flood stage this evening to a crest of 12.9 feet early Friday morning. It will then fall below flood stage late Saturday evening. - Flood stage is 9.0 feet. - http://www.weather.gov/safety/flood

INSTRUCTION: Motorists should not attempt to drive around barricades or drive cars through flooded areas. Additional information is available at www.weather.gov/ind. The next statement should be issued this evening by around 1115 PM EST.

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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.

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