Weather Alert in Kansas
Flood Warning issued August 27 at 7:56AM CDT until August 29 at 8:24PM CDT by NWS Wichita KS
AREAS AFFECTED: Allen, KS; Neosho, KS
DESCRIPTION: ...The National Weather Service in Wichita KS has issued a Flood Warning for the following rivers in Kansas... Cottonwood River near Plymouth affecting Lyon and Chase Counties. Neosho River near Chanute affecting Neosho and Allen Counties. Cottonwood River at Cottonwood Falls affecting Chase County. Cow Creek near Hutchinson affecting Reno and Rice Counties. * WHAT...Minor flooding is forecast. * WHERE...Neosho River near Chanute. * WHEN...From Thursday evening to Friday evening. * IMPACTS...At 23.0 feet, The right bank overflows and agricultural flooding can be expected. * ADDITIONAL DETAILS... - At 7:30 AM CDT Wednesday the stage was 8.6 feet. - Forecast...The river is expected to rise above flood stage late tomorrow evening to a crest of 23.8 feet early Friday morning. It will then fall below flood stage Friday morning. - Flood stage is 23.0 feet.
INSTRUCTION: Do not drive into flooded areas or go around barricades. Nearly two feet of water will carry most vehicles away. Turn around, don't drown. Additional information is available at www.weather.gov. The next statement will be issued this evening at 800 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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