Weather Alert in Indiana
Flood Warning issued March 4 at 10:54PM EST by NWS Indianapolis IN
AREAS AFFECTED: Daviess, IN; Gibson, IN; Knox, IN; Pike, IN
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Indiana... White River below Eagle Valley Power Plant. White River at Spencer. White River at Elliston. White River at Newberry. White River at Petersburg. ...The Flood Warning continues for the following rivers in Indiana... White River at Edwardsport. Youngs Creek at Amity. .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 forecast. * WHERE...White River at Petersburg. * WHEN...From Thursday evening until further notice. * IMPACTS...At 23.5 feet, Water from the Great June 2008 Flood recedes from SR 257 south of Washington. The river stage at Shoals was less than 10 feet and less than 14 feet previous day. The Lost River was low...except for backwater from the East Fork White...during this entire flood event. * ADDITIONAL DETAILS... - At 10:30 PM EST Wednesday /9:30 PM CST Wednesday/ the stage was 7.6 feet. - Forecast...The river is expected to rise above flood stage tomorrow evening and continue rising to a crest of 23.3 feet Tuesday morning. - Flood stage is 16.0 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 Thursday afternoon by around 200 PM EST /100 PM CST/.
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Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - 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
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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