Weather Alert in Indiana
Flood Warning issued March 4 at 10:51PM EST until March 5 at 10:00PM EST by NWS Indianapolis IN
AREAS AFFECTED: Clay, IN; Greene, IN
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Indiana... Buck Creek at Acton. Flatrock River at Saint Paul. East Fork White River at Columbus. ...The Flood Warning continues for the following rivers in Indiana... Flatrock River near Columbus. Driftwood River near Edinburgh. Big Blue River at Shelbyville. Eel River at Bowling Green. East Fork White River at Seymour. Clifty Creek at Hartsville. .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...Eel River at Bowling Green. * WHEN...Until late tomorrow evening. * IMPACTS...At 17.0 feet, Flood water covers considerable bottomlands and floods a few county roads including the Poland-Bowling Green Road. * ADDITIONAL DETAILS... - At 10:30 PM EST Wednesday the stage was 16.8 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 10:30 PM EST Wednesday was 17.4 feet. - Forecast...The river is expected to fall below flood stage late tomorrow morning and continue falling and remain below flood stage. - Flood stage is 15.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: 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 Thursday afternoon by around 145 PM EST.
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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
Weather Topic: What are Altostratus Clouds?
Home - Education - Cloud Types - Altostratus Clouds
Next Topic: Cirrocumulus Clouds
Altostratus clouds form at mid to high-level altitudes
(between 2 and 7 km) and are created by a warm, stable air mass which causes
water vapor
to condense as it rise through the atmosphere. Usually altostratus clouds are
featureless sheets characterized by a uniform color.
In some cases, wind punching through the cloud formation may give it a waved
appearance, called altostratus undulatus. Altostratus clouds
are commonly seen with other cloud formations accompanying them.
Next Topic: Cirrocumulus Clouds
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