Weather Alert in Indiana
Flood Advisory issued March 4 at 12:24AM EST until March 4 at 3:30AM EST by NWS Indianapolis IN
AREAS AFFECTED: Bartholomew, IN; Brown, IN; Decatur, IN; Jackson, IN; Jennings, IN; Johnson, IN; Monroe, IN; Morgan, IN; Shelby, IN
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall is expected. * WHERE...Bartholomew County in central Indiana... Decatur County in central Indiana... Southern Johnson County in central Indiana... Southeastern Morgan County in central Indiana... South Central Shelby County in central Indiana... Brown County in south central Indiana... Northern Jackson County in south central Indiana... East Central Monroe County in south central Indiana... Northern Jennings County in southeastern Indiana... * WHEN...Until 330 AM EST. * IMPACTS...Minor flooding in low-lying and poor drainage areas. * ADDITIONAL DETAILS... - At 1222 AM EST, Doppler radar and automated rain gauges indicated heavy rain due to thunderstorms. Minor flooding is ongoing or expected to begin shortly in the advisory area. Between 1 and 2.5 inches of rain have fallen. Rain is ongoing and an additional 1 to 2 inches of rain is possible. - Some locations that will experience flooding include... Columbus, Greensburg, North Vernon, Nashville, Edinburgh, Hope, Milford, Westport, Princes Lakes, Morgantown, Elizabethtown, Hartsville, Clifford, Jonesville, Millhousen, Azalia, Taylorsville, Newbern, Grammer and Waymansville. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Be especially cautious at night when it is harder to recognize the dangers of flooding.
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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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