Weather Alert in Kansas
Flood Warning issued March 7 at 8:30AM CST until March 10 at 10:42PM CDT by NWS Kansas City/Pleasant Hill MO
AREAS AFFECTED: Linn, KS
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Kansas... Marais Des Cygnes River at La Cygne affecting Linn County. * WHAT...Minor flooding is forecast. * WHERE...Marais Des Cygnes River at La Cygne. * WHEN...From this evening to late Tuesday evening. * IMPACTS...At 25.0 feet, Low lying farmland and other rural land floods. * ADDITIONAL DETAILS... - At 7:15 AM CST Saturday the stage was 22.7 feet. - Forecast...The river is expected to rise above flood stage this evening to a crest of 27.6 feet early Monday morning. It will then fall below flood stage late Monday evening. - Flood stage is 25.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. This product along with additional weather and stream information is available at www.weather.gov/kc/.
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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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