Weather Alert in Missouri
Flood Warning issued June 10 at 8:08AM CDT until June 15 at 7:00PM CDT by NWS Springfield MO
AREAS AFFECTED: St. Clair, MO; Vernon, MO
DESCRIPTION: ...The Flood Warning continues for the following rivers in Missouri... Little Osage River near Horton affecting Vernon County. Osage River at Taberville affecting St. Clair and Vernon Counties. ...The Flood Warning is extended for the following rivers in Missouri... Marmaton River near Nevada affecting Vernon County. For the Little Osage River...including Fulton, Horton...Minor flooding is forecast. For the Marmaton River...including Fort Scott, Nevada...Minor flooding is forecast. For the Osage River...including Taberville...Minor flooding is forecast. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Osage River at Taberville. * WHEN...Until Sunday evening. * IMPACTS...At 29.0 feet, flood waters impact B Highway 2.5 miles east of Rich Hill in the vicinity of the Bates County Drainage Ditch. * ADDITIONAL DETAILS... - At 7:45 AM CDT Tuesday the stage was 28.9 feet. - Bankfull stage is 23.0 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 7:45 AM CDT Tuesday was 28.9 feet. - Forecast...The river is expected to rise to a crest of 28.9 feet this afternoon. It will then fall below flood stage Saturday evening. - Flood stage is 23.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Many flood deaths occur in vehicles. Additional information is available at www.weather.gov. The next statement will be issued Wednesday morning at 815 AM CDT.
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Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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