Weather Alert in Missouri
Flood Advisory issued April 30 at 8:09AM CDT until May 3 at 1:00PM CDT by NWS Springfield MO
AREAS AFFECTED: Phelps, MO
DESCRIPTION: ...The National Weather Service in Springfield has issued a Flood Advisory for the following rivers in Missouri... Gasconade River at Jerome affecting Phelps County. For the Gasconade River...including Jerome...elevated river levels are forecast. * WHAT...Flooding caused by excessive rainfall is expected. * WHERE...Gasconade River at Jerome. * WHEN...From this morning to early Saturday afternoon. * IMPACTS...At 15.0 feet, minor flooding occurs near the gage site. Flood waters reach the lower edge of the concrete building where the gage equipment is located. * ADDITIONAL DETAILS... - At 7:45 AM CDT Wednesday the stage was 5.3 feet. - Bankfull stage is 15.0 feet. - Forecast...The river is expected to rise to a crest of 13.3 feet early Friday afternoon. - Action stage is 13.0 feet. - Flood stage is 15.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: If you encounter a flooded roadway, turn around and find an alternative route. Additional information is available at www.weather.gov. The next statement will be issued Thursday morning at 815 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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