Weather Alert in Indiana
Flood Warning issued March 4 at 12:07PM EST until March 8 at 12:00AM EST by NWS Indianapolis IN
AREAS AFFECTED: Bartholomew, IN
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Indiana... Big Blue River at Shelbyville. East Fork White River at Seymour. Flatrock River near Columbus. East Fork White River at Columbus. .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...Minor flooding is forecast. * WHERE...Flatrock River near Columbus. * WHEN...Until early Sunday morning. * IMPACTS...At 15.0 feet, Extensive flooding in progress along the Flatrock River. Portions of Riverside Drive north of US Highway 31 are flooded. According to the Columbus Response Plan... Indianapolis Road is flooded. * ADDITIONAL DETAILS... - At 11:30 AM EST Wednesday the stage was 9.5 feet. - Forecast...The river is expected to rise above flood stage this afternoon to a crest of 14.5 feet early tomorrow afternoon. It will then fall below flood stage Saturday evening. - Flood stage is 11.0 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 1115 PM EST.
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Weather Topic: What is Sleet?
Home - Education - Precipitation - Sleet
Next Topic: Snow
Sleet is a form of precipitation in which small ice pellets are the primary
components. These ice pellets are smaller and more translucent than hailstones,
and harder than graupel. Sleet is caused by specific atmospheric conditions and
therefore typically doesn't last for extended periods of time.
The condition which leads to sleet formation requires a warmer body of air to be
wedged in between two sub-freezing bodies of air. When snow falls through a warmer
layer of air it melts, and as it falls through the next sub-freezing body of air
it freezes again, forming ice pellets known as sleet. In some cases, water
droplets don't have time to freeze before reaching the surface and the result is
freezing rain.
Next Topic: Snow
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
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