Weather Alert in Indiana

Recent Locations: Schererville, IN  

Flood Warning issued July 2 at 8:54PM EDT until July 2 at 10:50PM EDT by NWS Indianapolis IN

AREAS AFFECTED: Daviess, IN; Gibson, IN; Knox, IN; Pike, IN

DESCRIPTION: ...The Flood Warning continues for the following river and locations in Indiana... White River at Hazleton and Petersburg. ...The Flood Warning is extended for the following river and location in Indiana... White River at Edwardsport. .Recent rainfall of 3 to 7 inches across the area over the past few days has created lowland flooding along the White River near Petersburg and Hazleton, where the crest has arrived. River flooding should end before the weekend arrives. * WHAT...No flooding is currently forecast. * WHERE...White River at Edwardsport. * WHEN...Until late this evening. * IMPACTS...At 12.0 feet, Water at this level prevents some fields from draining. * ADDITIONAL DETAILS... - At 7:00 PM EDT Wednesday /6:00 PM CDT Wednesday/ the stage was 13.0 feet. - Forecast...The river is expected to fall and remain below flood stage. - Flood stage is 15.0 feet. - http://www.weather.gov/safety/flood

INSTRUCTION: Be especially cautious at night when it is harder to recognize the dangers of flooding. Flooding is occurring or is imminent. Most flood related deaths occur in automobiles. Do not attempt to cross water covered bridges, dips, or low water crossings. Never try to cross a flowing stream, even a small one, on foot. To escape rising water find another route over higher ground. Additional information is available at www.weather.gov/ind. The next statement should be issued this evening by around 1100 PM EDT /1000 PM CDT/.

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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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