Weather Alert in Indiana
Flood Warning issued July 1 at 9:46PM EDT until July 3 at 3:00AM 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 Petersburg, Edwardsport, and Hazleton. .Rainfall amounts of 3 to 7 inches of rain fell across the area over the past few days. This will produce minor flooding along the White River near Edwardsport and points downstream in the coming days. River flooding should begin tonight and end by this weekend. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...White River at Edwardsport. * WHEN...Until early Thursday morning. * IMPACTS...At 16.0 feet, Old Vincennes Road and residential property in this area begin to flood. Flooding of low agricultural fields occurs along portions of the river. * ADDITIONAL DETAILS... - At 7:00 PM EDT Tuesday /6:00 PM CDT Tuesday/ the stage was 16.0 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 7:00 PM EDT Tuesday /6:00 PM CDT Tuesday/ was 16.0 feet. - Forecast...The river is expected to rise to a crest of 16.0 feet just after midnight tonight. It will then fall below flood stage tomorrow afternoon. - Flood stage is 15.0 feet. - 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. Additional information is available at www.weather.gov/ind. The next statement should be issued Wednesday afternoon by around 100 PM EDT /noon CDT/.
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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
Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
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