Weather Alert in Indiana
Flood Warning issued March 14 at 12:42PM EDT until March 19 at 10:00AM 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 Hazleton. White River at Petersburg. White River at Edwardsport. .Minor flooding on the White River from Edwardsport will continue through Thursday. Moderate flooding in progress on the lower White River at Petersburg and Hazleton will continue through early next week, with minor flooding of lowland areas persisting at Petersburg and Hazleton into early the following week. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...White River at Edwardsport. * WHEN...Until late Thursday morning. * IMPACTS...At 17.5 feet, Flooding closes Old Vincennes Road. High water crosses SR 358 on the Daviess County side just west of the levee. Flooding begins to affect higher bottomlands. Residential property of river cabins begins to flood. * ADDITIONAL DETAILS... - At 7:00 AM EDT Saturday /6:00 AM CDT Saturday/ the stage was 17.7 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 7:00 AM EDT Saturday /6:00 AM CDT Saturday/ was 18.3 feet. - Forecast...The river will fall below flood stage tomorrow afternoon to 12.8 feet Monday evening. It will then rise above flood stage early Wednesday morning to 15.3 feet early Wednesday afternoon. It will fall below flood stage again late Wednesday evening. - Flood stage is 15.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Caution is urged when walking near riverbanks. 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 late tonight by around 345 AM EDT /245 AM CDT/.
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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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