Weather Alert in Kansas
Flood Warning issued August 28 at 5:33AM CDT until August 28 at 2:00PM CDT by NWS Wichita KS
AREAS AFFECTED: Chautauqua, KS; Montgomery, KS
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall is possible. * WHERE...A portion of Southeast Kansas, including the following counties, Chautauqua and Montgomery. * WHEN...Until 200 PM CDT Thursday. * IMPACTS...Flooding of rivers, creeks, streams, city streets, and other low-lying and flood-prone locations is possible. * ADDITIONAL DETAILS... - At 533 AM CDT, Doppler radar indicated heavy rain due to thunderstorms. Up to 4 inches of rain has fallen overnight, with an additional 1 to 3 inches possible this morning. - Some locations that may experience flooding include... Coffeyville, Independence, Cherryvale, Caney, Sedan, Cedar Vale, Dearing, Elk City, Tyro, Peru, Liberty, Chautauqua, Havana, Elgin, Bolton, Sycamore, Niotaze, Hale, Independence Airport and Elk City 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. Be especially cautious at night when it is harder to recognize the dangers of flooding.
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Weather Topic: What are Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
Next Topic: Sleet
Weather Topic: What is Snow?
Home - Education - Precipitation - Snow
Next Topic: Stratocumulus Clouds
Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake,
has unique characteristics, but all of them grow in a hexagonal structure.
Snowfall can last for sustained periods of time and result in significant buildup
of snow on the ground.
On the earth's surface, snow starts out light and powdery, but as it begins to melt
it tends to become more granular, producing small bits of ice which have the consistency of
sand. After several cycles of melting and freezing, snow can become very dense
and ice-like, commonly known as snow pack.
Next Topic: Stratocumulus Clouds
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