Weather Alert in Kentucky
Special Weather Statement issued September 5 at 9:59PM EDT by NWS Jackson KY
AREAS AFFECTED: Montgomery; Bath; Powell
DESCRIPTION: At 959 PM EDT, Doppler radar was tracking a strong thunderstorm near Klondike, or 9 miles southwest of Mount Sterling, moving northeast at 30 mph. HAZARD...Wind gusts up to 40 mph and pea size hail. SOURCE...Radar indicated. IMPACT...Gusty winds could knock down tree limbs and blow around unsecured objects. Minor hail damage to vegetation is possible. Locations impacted include... Mount Sterling, Owingsville, Jeffersonville, Camargo, Sharpsburg, Preston, Reynoldsville, Levee, Sideview, Walkers Crossing, Flat Creek, Coons Station, Stepstone, Bourbon Furnace, Gatewoods Station, Prewitt, Crooks, Bethel, Stoops, and Peeled Oak. THIS INCLUDES THE FOLLOWING HIGHWAYS... Bert T. Combs Mountain Parkway between mile markers 12 and 13. Interstate 64 in eastern Kentucky between mile markers 105 and 123.
INSTRUCTION: If outdoors, consider seeking shelter inside a building. Torrential rainfall is also occurring with this storm and may lead to localized flooding. Do not drive your vehicle through flooded roadways. A Severe Thunderstorm Watch remains in effect until 100 AM EDT for east central Kentucky.
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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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