Weather Alert in Kansas
Severe Thunderstorm Warning issued September 3 at 7:10PM CDT until September 3 at 8:15PM CDT by NWS Wichita KS
AREAS AFFECTED: Sedgwick, KS
DESCRIPTION: SVRICT The National Weather Service in Wichita has issued a * Severe Thunderstorm Warning for... Sedgwick County in south central Kansas... * Until 815 PM CDT. * At 709 PM CDT, a severe thunderstorm was located over Bentley, or near Sedgwick, moving south at 35 mph. HAZARD...Tennis ball size hail and 70 mph wind gusts. SOURCE...Radar indicated. IMPACT...People and animals outdoors will be injured. Expect hail damage to roofs, siding, windows, and vehicles. Expect considerable tree damage. Wind damage is also likely to mobile homes, roofs, and outbuildings. * Locations impacted include... Wichita, Derby, Andover, Haysville, Park City, Valley Center, Bel Aire, Mulvane, Goddard, Rose Hill, Maize, Clearwater, Sedgwick, Colwich, Garden Plain, Mount Hope, Downtown Wichita, Kechi, Andale, and Eastborough. This includes the following highways... Interstate 135 between Mile Markers 0 and 22. Interstate 35 between Mile Markers 34 and 54.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building.
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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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