Weather Alert in Illinois
Flood Warning issued May 18 at 10:44AM CDT until May 21 at 7:00PM CDT by NWS Paducah KY
AREAS AFFECTED: Alexander, IL; Jackson, IL; Union, IL; Cape Girardeau, MO; Perry, MO; Scott, MO
DESCRIPTION: ...The Flood Warning continues for the following rivers in Kentucky...Missouri...Illinois... Mississippi River near Cape Girardeau and Hickman. .The Mississippi River levels will continue a slow fall, with the river falling below flood stage at Hickman later today, and at Cape Girardeau Tuesday afternoon. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Mississippi River at Cape Girardeau. * WHEN...Until Tuesday evening. * ADDITIONAL DETAILS... - At 10:30 AM CDT Saturday the stage was 32.9 feet. - Forecast...The river is expected to fall below flood stage early Tuesday afternoon and continue falling to 26.3 feet Tuesday, May 28. - Flood stage is 32.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Stay tuned to further developments by listening to your local radio, television, or NOAA Weather Radio for further information. Additional information is available at www.weather.gov.
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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
