Weather Alert in Indiana
Flood Warning issued June 6 at 11:33AM EDT until June 9 at 4:40PM 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 Newberry. White River at Edwardsport. White River at Elliston. ...The Flood Warning continues for the following rivers in Indiana... Wildcat Creek near Lafayette. Wabash River at Lafayette. .Rainfall amounts of two to four inches across central Indiana is producing minor flooding along area waterways in west-central Indiana. Additional rainfall of half an inch to an inch is possible over the White River basin through Sunday. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...White River at Edwardsport. * WHEN...Until Monday afternoon. * IMPACTS...At 18.0 feet, Old Vincennes Road and State Road 358 in Daviess County and Schaefer Road in Knox County are impassable. High water affects agricultural bottomlands. During agricultural season this level is of concern to farmers on the unprotected areas along the river. High water affects river cabins. * ADDITIONAL DETAILS... - At 7:00 AM EDT Friday /6:00 AM CDT Friday/ the stage was 15.4 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 7:00 AM EDT Friday /6:00 AM CDT Friday/ was 15.4 feet. - Forecast...The river is expected to rise to a crest of 18.1 feet tomorrow morning. It will then fall below flood stage early Monday morning. - 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 900 PM EDT /800 PM 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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