Weather Alert in Indiana
Flood Warning issued March 4 at 3:57AM EST until March 7 at 1:00AM EST by NWS Indianapolis IN
AREAS AFFECTED: Clay, IN; Greene, IN
DESCRIPTION: ...The National Weather Service in Indianapolis IN has issued a Flood Warning for the following rivers in Indiana... Big Blue River at Shelbyville. Driftwood River near Edinburgh. Flatrock River near Columbus. East Fork White River at Columbus. White River at Spencer. Eel River at Bowling Green. ...Forecast flooding changed from Minor to Moderate severity and increased in duration for the following rivers in Indiana... East Fork White River at Seymour. .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...Eel River at Bowling Green. * WHEN...From this afternoon to early Saturday morning. * IMPACTS...At 16.0 feet, Lowland flooding is occurring along portions of the river. Sonnefield Road at McIntyre Creek is impassable. Water is on portions of Pioneer Road in the vicinity of CR 50 N. This level threatens campers. * ADDITIONAL DETAILS... - At 3:30 AM EST Wednesday the stage was 12.6 feet. - Forecast...The river is expected to rise above flood stage this afternoon to a crest of 16.3 feet just after midnight tonight. It will then fall below flood stage early Friday afternoon. - 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. Additional information is available at www.weather.gov/ind. The next statement should be issued this evening by around 700 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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