Weather Alert in Kentucky
Special Weather Statement issued March 7 at 4:59PM EST by NWS Jackson KY
AREAS AFFECTED: Johnson; Magoffin; Floyd; Breathitt; Knott; Martin
DESCRIPTION: At 459 PM EST, Doppler radar was tracking strong thunderstorms along a line extending from Galen to near Daisydell. Movement was east at 45 mph. HAZARD...Wind gusts up to 40 mph. SOURCE...Radar indicated. IMPACT...Gusty winds could knock down tree limbs and blow around unsecured objects. Locations impacted include... Paintsville, Prestonsburg, Salyersville, Inez, Mason, Martin, Allen, Oaklawn Estates, Vail, Davella, Lancer, Falcon, Whitehouse, Burning Fork, Collista, West Van Lear, West Royalton Station, Williamsport, Blue River, and Milo. THIS INCLUDES THE FOLLOWING HIGHWAYS... Bert T. Combs Mountain Parkway between mile markers 72 and 76. Kentucky Highway 3 in Floyd County between mile markers 1 and 4. Kentucky Highway 3 in Johnson County Kentucky Highway 3 in Martin County between mile markers 1 and 9. Kentucky Highway 80 in Floyd County between mile markers 2 and 14. U.S. Highway 23 in Floyd County between mile markers 10 and 21. U.S. Highway 23 in Johnson County between mile markers 0 and 16.
INSTRUCTION: If outdoors, consider seeking shelter inside 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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