Weather Alert in Missouri
Flood Warning issued June 25 at 6:14AM CDT until June 28 at 8:50AM CDT by NWS Kansas City/Pleasant Hill MO
AREAS AFFECTED: Daviess, MO; Livingston, MO
DESCRIPTION: ...The Flood Warning continues for the following rivers in Missouri... Grand River near Gallatin affecting Daviess and Livingston Counties. Grand River near Pattonsburg affecting Daviess and Gentry Counties. Grand River near Chillicothe affecting Livingston and Linn Counties. Grand River near Sumner affecting Chariton, Linn, Livingston and Carroll Counties. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Grand River near Gallatin. * WHEN...Until Saturday morning. * IMPACTS...At 26.0 feet, low-lying woodlands and farmland along the river flood. * ADDITIONAL DETAILS... - At 5:45 AM CDT Wednesday the stage was 26.5 feet. - Forecast...The river is expected to rise to a crest of 29.5 feet tomorrow evening. It will then fall below flood stage Friday morning. - Flood stage is 26.0 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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