Weather Alert in Indiana
Flood Warning issued June 15 at 11:52AM EDT until June 16 at 9:42AM EDT by NWS Indianapolis IN
AREAS AFFECTED: Carroll, IN; Howard, IN
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Indiana... Wildcat Creek near Jerome to Lafayette. Wabash River at Montezuma. ...The Flood Warning continues for the following rivers in Indiana... White River at Ravenswood. .Rainfall amounts of 3 to 5 inches across portions of central Indiana late Friday into early Saturday continues to produce minor flooding along area creeks and rivers. Flooding along Wildcat Creek and Wabash River will gradually diminish over the next 24-48 hours. Flooding along the White River at Ravenswood will end by Sunday night. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Wildcat Creek at Kokomo. * WHEN...Until late tomorrow morning. * IMPACTS...At 12.0 feet, Wildcat Creek overflowing in parks in the Kokomo area. Flooding of agricultural land possible outside of Kokomo. * ADDITIONAL DETAILS... - At 11:00 AM EDT Sunday the stage was 11.3 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 11:00 AM EDT Sunday was 11.5 feet. - Forecast...The river is expected to fall below flood stage late tonight and continue falling and remain below flood stage. - Flood stage is 10.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Motorists should not attempt to drive around barricades or drive cars through flooded areas. 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 1215 AM EDT.
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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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