Weather Alert in Indiana
Flood Warning issued March 4 at 12:17PM EST until March 11 at 3:38AM 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 Newberry. * WHEN...From late tonight to Wednesday, March 11. * IMPACTS...At 20.0 feet, County Road 550 W in Green County is impassable. * ADDITIONAL DETAILS... - At 11:30 AM EST Wednesday the stage was 8.3 feet. - Forecast...The river is expected to rise above flood stage just after midnight tonight to a crest of 20.0 feet Saturday morning. It will then fall below flood stage Tuesday afternoon. - Flood stage is 13.0 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 are Wall Clouds?
Home - Education - Cloud Types - 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
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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