Weather Alert in Indiana
Flood Warning issued March 7 at 12:58PM EST by NWS Indianapolis IN
AREAS AFFECTED: Gibson, IN; Knox, IN
DESCRIPTION: ...The Flood Warning continues for the following rivers in Indiana... Illinois... White River at Edwardsport, Spencer, Newberry, Elliston, Hazleton, and Petersburg. Wabash River at Mount Carmel. .Total rainfall amounts of 3 to over 5 inches of rain across much of central and southern Indiana is bringing widespread moderate flooding across the East Fork White and lower White basins and their tributaries. Minor flooding is expected in the lowest reach of the Wabash River at Mount Carmel starting Saturday night. Additional rainfall earlier today and next week could lengthen the amount of time area rivers remain in flood or bring additional rises next week. * WHAT...Moderate flooding is forecast. * WHERE...White River at Hazleton. * WHEN...Until further notice. * IMPACTS...At 24.8 feet, Water begins to come in the street at the corner of West 2nd Street and Brown Street in the town of Hazleton. A six inch water pump is installed at 2nd and Brown Street to keep water off the streets. * ADDITIONAL DETAILS... - There is no current observed data. - Forecast...The river is expected to rise to a crest of 24.4 feet early Wednesday morning. - Flood stage is 16.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Flooding is occurring or is imminent. Most flood related deaths occur in automobiles. Do not attempt to cross water covered bridges, dips, or low water crossings. Never try to cross a flowing stream, even a small one, on foot. To escape rising water find another route over higher ground. Caution is urged when walking near riverbanks. Additional information is available at www.weather.gov/ind. The next statement should be issued late tonight by around 500 AM EDT /400 AM CDT/.
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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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