Weather Alert in Missouri
Severe Thunderstorm Warning issued March 6 at 7:40PM CST until March 6 at 8:15PM CST by NWS Kansas City/Pleasant Hill MO
AREAS AFFECTED: Bates, MO; Cass, MO; Henry, MO
DESCRIPTION: SVREAX The National Weather Service in Pleasant Hill has issued a * Severe Thunderstorm Warning for... Southeastern Cass County in west central Missouri... Northwestern Henry County in west central Missouri... Central Bates County in west central Missouri... * Until 815 PM CST. * At 739 PM CST, a severe thunderstorm was located near Butler, moving northeast at 50 mph. HAZARD...60 mph wind gusts and quarter size hail. SOURCE...Radar indicated. IMPACT...Hail damage to vehicles is expected. Expect wind damage to roofs, siding, and trees. * Locations impacted include... Butler, Adrian, Garden City, Archie, Urich, Creighton, Amoret, Foster, Blairstown, Passaic, Ballard, and Worland. This includes Interstate 49 between mile markers 125 and 153.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building. A Tornado Watch remains in effect until 100 AM CST for east central Kansas...and west central Missouri.
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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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