Weather Alert in Arkansas
Flood Advisory issued May 31 at 8:51PM CDT until June 16 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...Mississippi...Louisiana... Mississippi River Near Greenville affecting East Carroll, Issaquena, Chicot and Washington Counties. Mississippi River At Natchez affecting Concordia, Adams and Wilkinson Counties. Mississippi River At Vicksburg affecting Claiborne, Madison, Tensas, Jefferson and Warren Counties. * WHAT...Flooding caused by excessive rainfall continues. * WHERE...Mississippi River near Greenville. * WHEN...Until Monday, June 16. * IMPACTS...At 42.0 feet, Flooding is occurring around Lake Ferguson. * ADDITIONAL DETAILS... - At 11:00 AM CDT Saturday the stage was 41.6 feet. - Forecast...The river is expected to fall to 29.0 feet Saturday, June 28. - 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 Sunday morning at 900 AM CDT.
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Weather Topic: What is Sleet?
Home - Education - Precipitation - Sleet
Next Topic: Snow
Sleet is a form of precipitation in which small ice pellets are the primary
components. These ice pellets are smaller and more translucent than hailstones,
and harder than graupel. Sleet is caused by specific atmospheric conditions and
therefore typically doesn't last for extended periods of time.
The condition which leads to sleet formation requires a warmer body of air to be
wedged in between two sub-freezing bodies of air. When snow falls through a warmer
layer of air it melts, and as it falls through the next sub-freezing body of air
it freezes again, forming ice pellets known as sleet. In some cases, water
droplets don't have time to freeze before reaching the surface and the result is
freezing rain.
Next Topic: Snow
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
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