Weather Alert in Indiana
Flood Warning issued March 4 at 3:57AM EST by NWS Indianapolis IN
AREAS AFFECTED: Johnson, IN
DESCRIPTION: ...The Flood Warning continues for the following rivers in Indiana... Haw Creek near Clifford. White River at Elliston. Youngs Creek at Amity. ...The Flood Warning is extended for the following rivers in Indiana... White River at Newberry. .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 occurring and minor flooding is forecast. * WHERE...Youngs Creek at Amity. * WHEN...Until further notice. * IMPACTS...At 10.0 feet, Significant flooding in progress. Parks and some local roads are flooded by a foot or more of water. Agricultural flooding is noticeable. * ADDITIONAL DETAILS... - At 3:15 AM EST Wednesday the stage was 9.2 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 3:15 AM EST Wednesday was 9.2 feet. - Forecast...The river is expected to rise to 9.9 feet this afternoon. Additional rises are possible thereafter. - Flood stage is 7.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Stay tuned to further developments by listening to your local radio, television, or NOAA Weather Radio for further information. Be especially cautious at night when it is harder to recognize the dangers of flooding. Additional information is available at www.weather.gov/ind. The next statement should be issued this afternoon by around 330 PM EST.
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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.
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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.
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