Weather Alert in Kansas
Flood Warning issued August 31 at 8:03PM CDT until September 1 at 9:30PM CDT by NWS Wichita KS
AREAS AFFECTED: Marion, KS
DESCRIPTION: ...The Flood Warning continues for the following rivers in Kansas... Cottonwood River near Florence affecting Marion County. * WHAT...Minor flooding is forecast. * WHERE...Cottonwood River near Florence. * WHEN...From this evening to late tomorrow evening. * IMPACTS...At 24.0 feet, Outside the levee system in southeast Florence, flood waters flow across Park Ave Road and reach the foundation of a residential home. Northwest of Florence, the bridge on 140th Road and 1/2 mile west of Highway 77 floods. * ADDITIONAL DETAILS... - At 7:15 PM CDT Sunday the stage was 19.3 feet and rising. - Forecast...The river is expected to rise above flood stage late this evening to a crest of 23.2 feet just after midnight tonight. It will then fall below flood stage late tomorrow morning. - Flood stage is 22.0 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 Monday morning at 815 AM CDT.
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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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