Weather Alert in Indiana
Flood Warning issued June 10 at 12:13PM EDT until June 12 at 7:00PM EDT by NWS Indianapolis IN
AREAS AFFECTED: Daviess, IN; Greene, IN; Knox, IN
DESCRIPTION: ...The Flood Warning continues for the following rivers in Indiana... White River at Newberry, Petersburg, Hazleton, Edwardsport, and Elliston. .Rainfall amounts within the past few days of two to four inches across central Indiana is producing minor flooding along the White River in western Indiana. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...White River at Elliston. * WHEN...Until Thursday evening. * IMPACTS...At 21.0 feet, Eastern portion of CR 100 S in Greene County floods leading to Plummer. Flooding covers all low bottomlands. * ADDITIONAL DETAILS... - At 8:00 AM EDT Tuesday the stage was 20.4 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 8:00 AM EDT Tuesday was 20.4 feet. - Forecast...The river is expected to rise to a crest of 20.6 feet this afternoon. It will then fall below flood stage Thursday morning. - Flood stage is 18.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Additional information is available at www.weather.gov/ind. The next statement should be issued late tonight by around 315 AM EDT /215 AM 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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