Weather Alert in Indiana
Flood Warning issued May 8 at 11:11PM EDT until May 9 at 6:00PM EDT by NWS Indianapolis IN
AREAS AFFECTED: Gibson, IN; Knox, IN
DESCRIPTION: ...The Flood Warning is extended for the following river in Indiana... White River at Hazleton. .Rainfall over the last several days has caused minor flooding at Hazleton. Flooding is expected to end late tonight. * WHAT...Minor flooding is forecast. * WHERE...White River at Hazleton. * WHEN...Until tomorrow evening. * IMPACTS...At 16.0 feet, Flooding begins in lowest bottomlands and a few local roads. High water affects a few low oil fields. * ADDITIONAL DETAILS... - There is no current observed data. - Forecast...The river is expected to fall below flood stage tomorrow morning and continue falling and remain below flood stage. - Flood stage is 16.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Be especially cautious at night when it is harder to recognize the dangers of flooding. Flooding is occurring or is imminent. Most flood related deaths occur in automobiles. Do not attempt to cross water covered bridges, dips, or low water crossings. Never try to cross a flowing stream, even a small one, on foot. To escape rising water find another route over higher ground. Additional information is available at www.weather.gov/ind. The next statement should be issued Friday afternoon by around 215 PM EDT /115 PM CDT/.
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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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