Weather Alert in Indiana
Flood Warning issued March 5 at 10:57PM EST until March 14 at 2:00AM EDT 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 at Edwardsport, Newberry, Elliston, and Hazleton. ...The Flood Warning continues for the following rivers in Indiana... White River at Spencer and Petersburg. .Total rainfall amounts of 3 to over 5 inches of rain across much of central and southern Indiana is bringing widespread flooding. Additional rainfall over the weekend and next week could lengthen the amount of time the river remains in flood. * WHAT...Minor flooding is occurring and moderate flooding is forecast. * WHERE...White River at Edwardsport. * WHEN...Until Saturday, March 14. * IMPACTS...At 22.9 feet, A 25 foot section of Levee Unit 8 failed at this level on March 6 2011...flooding local roads behind the levee. Flooding not nearly as bad as June 2008 levee failure. * ADDITIONAL DETAILS... - At 7:00 PM EST Thursday /6:00 PM CST Thursday/ the stage was 17.6 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 7:00 PM EST Thursday /6:00 PM CST Thursday/ was 17.6 feet. - Forecast...The river is expected to rise to a crest of 22.1 feet Sunday evening. It will then fall below flood stage Friday, March 13. - Flood stage is 15.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Motorists should not attempt to drive around barricades or drive cars through flooded areas. 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 Friday 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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