Weather Alert in Missouri
Flood Warning issued April 30 at 8:25AM CDT until May 3 at 8:30AM CDT by NWS Springfield MO
AREAS AFFECTED: Shannon, MO
DESCRIPTION: ...The National Weather Service in Springfield MO has issued a Flood Warning for the following rivers in Missouri... Current River near Powder Mill affecting Shannon County. For the Current River...including Powder Mill...Minor flooding is forecast. * WHAT...Minor flooding is forecast. * WHERE...Current River near Powder Mill. * WHEN...From late tonight to Saturday morning. * IMPACTS...At 8.0 feet, County Road 106-531 south of the gage floods near the river. * ADDITIONAL DETAILS... - At 7:45 AM CDT Wednesday the stage was 5.4 feet. - Bankfull stage is 8.0 feet. - Forecast...The river is expected to rise above flood stage late tonight to a crest of 9.0 feet early tomorrow afternoon. It will then fall below flood stage Friday morning. - Flood stage is 8.0 feet. - Flood History...This crest compares to a previous crest of 9.7 feet on 05/28/2016. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Many flood deaths occur in vehicles. Additional information is available at www.weather.gov. The next statement will be issued Thursday morning at 830 AM 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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