Weather Alert in Kansas
Flood Warning issued August 11 at 1:32AM CDT until August 11 at 10:30AM CDT by NWS Wichita KS
AREAS AFFECTED: Butler, KS; Chase, KS; Greenwood, KS
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall is expected. * WHERE...Portions of Central, South Central, and Southeast Kansas, including the following counties, in Central Kansas, Chase. In South Central Kansas, Butler. In Southeast Kansas, Greenwood. * WHEN...Until 1030 AM CDT Monday. * IMPACTS...Flooding of rivers, creeks, streams, and other low-lying and flood-prone locations is imminent or occurring. * ADDITIONAL DETAILS... - At 132 AM CDT, Doppler radar indicated heavy rain due to thunderstorms. Flooding is ongoing or expected to begin shortly in the warned area. - Some locations that will experience flooding include... Eureka, Cottonwood Falls, Madison, Strong City, Hamilton, Rosalia, Cassoday, Bazaar, Climax, Virgil, Elmdale, Matfield Green, Cedar Point, Thrall, Eureka City Lake, Eureka Airport, Saffordville, Wonsevu, El Dorado State Park and El Dorado Lake.
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.
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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
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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