Weather Alert in Indiana

Recent Locations: Granite Quarry, NC   Chandler, IN  

Flood Warning issued June 30 at 12:01PM EDT until July 2 at 5:00PM EDT by NWS Indianapolis IN

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

DESCRIPTION: ...The National Weather Service in Indianapolis IN has issued a Flood Warning for the following rivers in Indiana... White River at Edwardsport. .Rainfall amounts of 2 to 6 inches of rain fell across the area and upstream over the weekend. This will produce minor flooding along the White River near Edwardsport and possibly downstream in the coming days. River flooding should begin tonight and end by midweek. There are chances for additional isolated showers through this evening. * WHAT...Minor flooding is forecast. * WHERE...White River at Edwardsport. * WHEN...From this evening to Wednesday afternoon. * IMPACTS...At 16.0 feet, Old Vincennes Road and residential property in this area begin to flood. Flooding of low agricultural fields occurs along portions of the river. * ADDITIONAL DETAILS... - At 7:00 AM EDT Monday /6:00 AM CDT Monday/ the stage was 11.5 feet. - Forecast...The river is expected to rise above flood stage late this evening to a crest of 16.3 feet early tomorrow afternoon. It will then fall below flood stage early Wednesday morning. - Flood stage is 15.0 feet. - http://www.weather.gov/safety/flood

INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Additional information is available at www.weather.gov/ind. The next statement should be issued late tonight by around 315 AM EDT /215 AM CDT/.

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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

Weather Topic: What are Altostratus Clouds?

Home - Education - Cloud Types - Altostratus Clouds

Altostratus Clouds Next Topic: Cirrocumulus Clouds

Altostratus clouds form at mid to high-level altitudes (between 2 and 7 km) and are created by a warm, stable air mass which causes water vapor to condense as it rise through the atmosphere. Usually altostratus clouds are featureless sheets characterized by a uniform color.

In some cases, wind punching through the cloud formation may give it a waved appearance, called altostratus undulatus. Altostratus clouds are commonly seen with other cloud formations accompanying them.

Next Topic: Cirrocumulus Clouds

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