Weather Alert in Arkansas
Flood Advisory issued June 26 at 8:59PM CDT until July 14 at 1:00AM CDT by NWS Jackson MS
AREAS AFFECTED: Chicot, AR; East Carroll, LA; Issaquena, MS; Washington, MS
DESCRIPTION: ...The Flood Advisory is extended for the following rivers in Louisiana...Arkansas...Mississippi... Mississippi River Near Greenville affecting Washington, Chicot, Issaquena and East Carroll Counties. Mississippi River At Natchez affecting Adams, Wilkinson and Concordia Counties. ...The Flood Advisory continues for the following rivers in Louisiana...Mississippi... Mississippi River At Vicksburg affecting Warren, Madison, Jefferson, Tensas and Claiborne Counties. * WHAT...Flooding caused by excessive rainfall continues. * WHERE...Mississippi River near Greenville. * WHEN...Until Monday, July 14. * IMPACTS...At 42.0 feet, Flooding is occurring around Lake Ferguson. * ADDITIONAL DETAILS... - At 8:00 PM CDT Thursday the stage was 41.7 feet. - Forecast...The river is expected to rise to a crest of 41.8 feet just after midnight tonight. - Action stage is 36 feet. - Flood stage is 48 feet.
INSTRUCTION: If you encounter a flooded roadway, turn around and find an alternative route. The next statement will be issued Friday morning at 900 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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