Weather Alert in Arkansas
Flood Warning issued April 24 at 11:50AM CDT by NWS Memphis TN
AREAS AFFECTED: Lee, AR; St. Francis, AR
DESCRIPTION: ...The Flood Warning continues for the following rivers in Arkansas... L'Anguille River at Palestine For the L'anguille River...including Palestine...Minor flooding is forecast. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...L'Anguille River at Palestine. * WHEN...Until further notice. * IMPACTS...At 26.0 feet, Flooding is occurring in low-lying farmland near the river. * ADDITIONAL DETAILS... - At 10:00 AM CDT Thursday the stage was 26.6 feet. - Forecast...The river will continue to gradually fall into next week, but remain in Minor Flood Stage. - Flood stage is 25.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Motorists should not attempt to drive around barricades or drive cars through flooded areas. Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Additional information is available at weather.gov/memphis. The next statement will be issued as needed.
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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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