Weather Alert in Indiana

Recent Locations: Griffin, GA   Wabash, IN   Trimont, MN  

Flood Warning issued March 4 at 3:57AM EST by NWS Indianapolis IN

AREAS AFFECTED: Johnson, IN

DESCRIPTION: ...The Flood Warning continues for the following rivers in Indiana... Haw Creek near Clifford. White River at Elliston. Youngs Creek at Amity. ...The Flood Warning is extended for the following rivers in Indiana... White River at Newberry. .Between 2 and 4 inches of rain have fallen across central Indiana as of early Wednesday morning. Up to 2 inches have fallen in south-central Indiana. This has led creeks to rise above flood stage and rivers will follow in the coming days. Additional rain is in the forecast over the next several days. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Youngs Creek at Amity. * WHEN...Until further notice. * IMPACTS...At 10.0 feet, Significant flooding in progress. Parks and some local roads are flooded by a foot or more of water. Agricultural flooding is noticeable. * ADDITIONAL DETAILS... - At 3:15 AM EST Wednesday the stage was 9.2 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 3:15 AM EST Wednesday was 9.2 feet. - Forecast...The river is expected to rise to 9.9 feet this afternoon. Additional rises are possible thereafter. - Flood stage is 7.0 feet. - http://www.weather.gov/safety/flood

INSTRUCTION: Stay tuned to further developments by listening to your local radio, television, or NOAA Weather Radio for further information. Be especially cautious at night when it is harder to recognize the dangers of flooding. Additional information is available at www.weather.gov/ind. The next statement should be issued this afternoon by around 330 PM EST.

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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

Weather Topic: What are Wall Clouds?

Home - Education - Cloud Types - Wall Clouds

Wall Clouds Next Topic: Altocumulus Clouds

A wall cloud forms underneath the base of a cumulonimbus cloud, and can be a hotbed for deadly tornadoes.

Wall clouds are formed by air flowing into the cumulonimbus clouds, which can result in the wall cloud descending from the base of the cumulonimbus cloud, or rising fractus clouds which join to the base of the storm cloud as the wall cloud takes shape.

Wall clouds can be very large, and in the Northern Hemisphere they generally form at the southern edge of cumulonimbus clouds.

Next Topic: Altocumulus Clouds

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