Weather Alert in Illinois
Flood Warning issued April 28 at 8:07PM CDT until May 2 at 7:00AM CDT by NWS Paducah KY
AREAS AFFECTED: Gallatin, IL; Wayne, IL; White, IL
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Illinois... Little Wabash River at Carmi .Minor flooding continues on the Little Wabash River at Carmi. Water levels continue to slowly fall, and the river is forecast to fall below flood stage early Friday morning. For the Little Wabash River...including Carmi...Minor flooding is forecast. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Little Wabash River at Carmi. * WHEN...Until Friday morning. * IMPACTS...At 27.0 feet, The inundation of county roads begins. * ADDITIONAL DETAILS... - At 7:30 PM CDT Monday the stage was 28.8 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 7:30 PM CDT Monday was 29.2 feet. - Forecast...The river is expected to fall below flood stage early Friday morning and continue falling to 22.2 feet Monday, May 05. - Flood stage is 27.0 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.
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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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