Weather Alert in Missouri
Flood Advisory issued April 25 at 9:35PM CDT until April 27 at 7:00AM CDT by NWS Memphis TN
AREAS AFFECTED: New Madrid, MO; Pemiscot, MO; Lake, TN
DESCRIPTION: ...The Flood Advisory continues for the following rivers in Arkansas...Tennessee...Mississippi...Missouri... Mississippi River at Memphis Mississippi River Above Tiptonville For the Lower Mississippi River...including Tiptonville, Caruthersville, Osceola, Memphis, Tunica Mhoon Landing, Helena... elevated river levels are forecast. * WHAT...Flooding caused by excessive rainfall continues. * WHERE...Mississippi River above Tiptonville. * WHEN...Until Sunday morning. * IMPACTS...At 36.0 feet, In Missouri, most fields around Robinson Lake in Pemiscot County are covered by flood water. * ADDITIONAL DETAILS... - At 9:00 PM CDT Friday the stage was 36.0 feet. - Forecast...The river is expected to fall to 23.7 feet Monday, May 05. - Action stage is 34.0 feet. - Flood stage is 37.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Caution is urged when walking near riverbanks. Additional information is available at weather.gov/memphis. The next statement will be issued as needed.
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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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