Weather Alert in Kansas
Flood Warning issued August 31 at 12:40PM CDT until September 1 at 10:00AM CDT by NWS Wichita KS
AREAS AFFECTED: McPherson, KS; Marion, KS
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall is expected. * WHERE...A portion of Central Kansas, including the following counties, Marion and McPherson. * WHEN...Until 1000 AM CDT Monday. * IMPACTS...Flooding of rivers, creeks, streams, and other low-lying and flood-prone locations is imminent or occurring. Numerous roads remain closed due to flooding. * ADDITIONAL DETAILS... - At 1233 PM CDT, local law enforcement reported multiple roads closed due to flooding in McPherson and Marion counties. Between 2 and 4 inches of rain have fallen. - Some locations that will experience flooding include... Mcpherson, Hillsboro, Moundridge, Inman, Galva, Canton, Goessel, Lehigh, Windom and Mcpherson Airport.
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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