Weather Alert in Missouri
Flood Warning issued July 17 at 9:41AM CDT until July 19 at 1:37PM CDT by NWS Kansas City/Pleasant Hill MO
AREAS AFFECTED: Jackson, MO; Lafayette, MO; Ray, MO
DESCRIPTION: ...The National Weather Service in Pleasant Hill MO has issued a Flood Warning for the following rivers in Missouri... Missouri River at Napoleon affecting Jackson, Ray and Lafayette Counties. Missouri River at Waverly affecting Lafayette, Carroll and Saline Counties. Missouri River At Miami affecting Carroll, Saline and Chariton Counties. * WHAT...Minor flooding is forecast. * WHERE...Missouri River at Napoleon. * WHEN...From this evening to early Saturday afternoon. * IMPACTS...At 17.0 feet, Low-lying areas unprotected by levees begin to flood. * ADDITIONAL DETAILS... - At 9:00 AM CDT Thursday the stage was 11.9 feet. - Forecast...The river is expected to rise above flood stage late this evening to a crest of 17.7 feet tomorrow morning. It will then fall below flood stage early tomorrow afternoon. - Flood stage is 17.0 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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