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 Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
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