Weather Alert in Kansas
Flood Warning issued August 11 at 8:13AM CDT until August 14 at 2:43PM CDT by NWS Wichita KS
AREAS AFFECTED: Reno, KS; Rice, KS
DESCRIPTION: ...The National Weather Service in Wichita KS has issued a Flood Warning for the following rivers in Kansas... Cow Creek near Hutchinson affecting Reno and Rice Counties. * WHAT...Minor flooding is forecast. * WHERE...Cow Creek near Hutchinson. * WHEN...From Tuesday morning to early Thursday afternoon. * IMPACTS...At 10.0 feet, The low water crossing on Wilson Rd between 69th Ave to 82nd Ave floods. Expect water depth near 4 inches to a width of 5 feet. * ADDITIONAL DETAILS... - At 7:15 AM CDT Monday the stage was 5.3 feet. - Forecast...The river is expected to rise above flood stage late tomorrow morning to a crest of 10.0 feet Wednesday morning. It will then fall below flood stage early Thursday morning. - Flood stage is 9.5 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. Motorists should not attempt to drive around barricades or drive cars through flooded areas. Additional information is available at www.weather.gov. The next statement will be issued this evening at 815 PM 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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