Weather Alert in Arkansas
Flood Warning issued April 27 at 9:05PM CDT by NWS Shreveport LA
AREAS AFFECTED: Ashley, AR; Union, AR
DESCRIPTION: ...The Flood Warning continues for the following rivers in Arkansas... Ouachita River At Felsenthal Lock and Dam affecting Union and Ashley Counties. For the Ouachita River...including Felsenthal Lock and Dam, Monroe, Columbia...Minor flooding is forecast. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Ouachita River at Felsenthal Lock and Dam. * WHEN...Until further notice. * ADDITIONAL DETAILS... - At 8:30 PM CDT Sunday the stage was 75.8 feet. - Bankfull stage is 65.0 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 8:30 PM CDT Sunday was 76.1 feet. - Forecast...The river is expected to fall to 74.1 feet Friday evening. - Flood stage is 70.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Do not drive cars through flooded areas. Caution is urged when walking near riverbanks. Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Motorists should not attempt to drive around barricades or drive cars through flooded areas. The next statement will be issued Monday evening at 915 PM CDT.
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Weather Topic: What are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
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