Weather Alert in Arkansas
Flood Advisory issued May 27 at 11:04AM CDT until June 11 at 7:00PM CDT by NWS Jackson MS
AREAS AFFECTED: Chicot, AR; East Carroll, LA; Issaquena, MS; Washington, MS
DESCRIPTION: ...The Flood Advisory continues for the following rivers in Arkansas...Louisiana...Mississippi... Mississippi River Near Greenville affecting Issaquena, Washington, East Carroll and Chicot Counties. Mississippi River At Natchez affecting Adams, Wilkinson and Concordia Counties. Mississippi River At Vicksburg affecting Claiborne, Jefferson, Tensas, Madison and Warren Counties. * WHAT...Flooding caused by excessive rainfall continues. * WHERE...Mississippi River near Greenville. * WHEN...Until Wednesday, June 11. * IMPACTS...At 42.0 feet, Flooding is occurring around Lake Ferguson. * ADDITIONAL DETAILS... - At 10:00 AM CDT Tuesday the stage was 40.4 feet. - Forecast...The river is expected to rise to a crest of 41.0 feet tomorrow evening. - Action stage is 36.0 feet. - Flood stage is 48.0 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.water.noaa.gov/wfo/jan The next statement will be issued this evening at 1115 PM 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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