Weather Alert in Arkansas
Flood Advisory issued May 31 at 7:50PM CDT until June 3 at 1:00PM CDT by NWS Tulsa OK
AREAS AFFECTED: Franklin, AR; Johnson, AR; Logan, AR
DESCRIPTION: ...The Flood Advisory continues for the following rivers in Arkansas... Arkansas River at Ozark Lock and Dam affecting Johnson, Franklin and Logan Counties. * WHAT...Flooding caused by excessive rainfall continues. * WHERE...Arkansas River at Ozark Lock and Dam. * WHEN...Until early Tuesday afternoon. * IMPACTS...At 355.5 feet, the river remains in its banks, but access to Okane Island may be cut off. * ADDITIONAL DETAILS... - At 7:00 PM CDT Saturday the stage was 354.4 feet. - Forecast...The river is expected to rise above action stage by Sunday afternoon and to a crest of 355.6 feet early Monday afternoon. - Action stage is 355.5 feet. - Flood stage is 357.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: N/A
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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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