Weather Alert in Indiana

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Flood Warning issued March 4 at 12:17PM EST until March 11 at 1:15PM EDT by NWS Indianapolis IN

AREAS AFFECTED: Daviess, IN; Greene, IN; Knox, IN

DESCRIPTION: ...The National Weather Service in Indianapolis IN has issued a Flood Warning for the following rivers in Indiana... White River below Eagle Valley Power Plant. White River near Centerton. White River at Edwardsport. White River at Petersburg. ...Forecast flooding changed from Minor to Moderate severity and increased in duration for the following rivers in Indiana... White River at Elliston. White River at Newberry. .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...Moderate flooding is forecast. * WHERE...White River at Elliston. * WHEN...From this afternoon to Wednesday, March 11. * IMPACTS...At 26.0 feet, Shawnee Airfield floods as flood waters begin to get into the hangar. Relocation of livestock may be necessary. * ADDITIONAL DETAILS... - There is no current observed data. - Forecast...The river is expected to rise above flood stage late this afternoon to a crest of 25.8 feet Saturday morning. It will then fall below flood stage Wednesday, March 11. - Flood stage is 18.0 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 1130 PM EST /1030 PM CST/.

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Weather Topic: What is Sleet?

Home - Education - Precipitation - Sleet

Sleet Next Topic: Snow

Sleet is a form of precipitation in which small ice pellets are the primary components. These ice pellets are smaller and more translucent than hailstones, and harder than graupel. Sleet is caused by specific atmospheric conditions and therefore typically doesn't last for extended periods of time.

The condition which leads to sleet formation requires a warmer body of air to be wedged in between two sub-freezing bodies of air. When snow falls through a warmer layer of air it melts, and as it falls through the next sub-freezing body of air it freezes again, forming ice pellets known as sleet. In some cases, water droplets don't have time to freeze before reaching the surface and the result is freezing rain.

Next Topic: Snow

Weather Topic: What are Stratocumulus Clouds?

Home - Education - Cloud Types - Stratocumulus Clouds

Stratocumulus Clouds Next Topic: Stratus Clouds

Stratocumulus clouds are similar to altocumulus clouds in their fluffy appearance, but have a slightly darker shade due to their additional mass.

A good way to distinguish the two cloud types is to hold your hand out and measure the size of an individual cloud; if it is the size of your thumb it is generally an altocumulus cloud, if it is the size of your hand it is generally a stratocumulus cloud.

It is uncommon for stratocumulus clouds to produce precipitation, but if they do it is usually a light rain or snow.

Next Topic: Stratus Clouds

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