Weather Alert in Kansas
Severe Thunderstorm Warning issued August 3 at 7:25PM CDT until August 3 at 8:30PM CDT by NWS Dodge City KS
AREAS AFFECTED: Clark, KS; Ford, KS; Gray, KS; Kiowa, KS; Meade, KS
DESCRIPTION: SVRDDC The National Weather Service in Dodge City has issued a * Severe Thunderstorm Warning for... Ford County in southwestern Kansas... Southwestern Kiowa County in south central Kansas... Northeastern Meade County in southwestern Kansas... Southeastern Gray County in southwestern Kansas... Northern Clark County in southwestern Kansas... * Until 830 PM CDT. * At 725 PM CDT, a severe thunderstorm was located near Dodge City, moving south at 30 mph. THIS IS A DESTRUCTIVE STORM FOR Ford county. HAZARD...90 mph wind gusts and half dollar size hail. SOURCE...Radar indicated. IMPACT...You are in a life-threatening situation. Flying debris may be deadly to those caught without shelter. Mobile homes will be heavily damaged or destroyed. Homes and businesses will have substantial roof and window damage. Expect extensive tree damage and power outages. * This severe thunderstorm will be near... Minneola around 745 PM CDT.
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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