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 Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
Next Topic: Sleet
Weather Topic: What is Snow?
Home - Education - Precipitation - Snow
Next Topic: Stratocumulus Clouds
Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake,
has unique characteristics, but all of them grow in a hexagonal structure.
Snowfall can last for sustained periods of time and result in significant buildup
of snow on the ground.
On the earth's surface, snow starts out light and powdery, but as it begins to melt
it tends to become more granular, producing small bits of ice which have the consistency of
sand. After several cycles of melting and freezing, snow can become very dense
and ice-like, commonly known as snow pack.
Next Topic: Stratocumulus Clouds
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