Weather Alert in Kentucky
Special Weather Statement issued September 5 at 9:53PM EDT by NWS Jackson KY
AREAS AFFECTED: Rockcastle; Jackson; Pulaski; Laurel
DESCRIPTION: At 953 PM EDT, Doppler radar was tracking strong thunderstorms along a line extending from Morrill to near Dabney. Movement was east at 50 mph. HAZARD...Wind gusts up to 50 mph and penny size hail. SOURCE...Radar indicated. IMPACT...Gusty winds could knock down tree limbs and blow around unsecured objects. Minor damage to outdoor objects is possible. Locations impacted include... Mount Vernon, McKee, Boone, Science Hill, Donaro, Bummer, Robinet, Gum Sulphur, Shop Branch, Bandy, Privett, Horse Lick, Spiro, Climax, Renfro Valley, Disputanta, Mershons, Hazel Patch, Pine Hill, and Camp Wildcat. THIS INCLUDES THE FOLLOWING HIGHWAYS... Interstate 75 in east central Kentucky between mile markers 42 and 72. Kentucky Highway 80 in Laurel County between mile markers 1 and 10. Kentucky Highway 80 in Pulaski County between mile markers 26 and 40.
INSTRUCTION: If outdoors, consider seeking shelter inside a building. Torrential rainfall is also occurring with these storms 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 south central and southeastern Kentucky.
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Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
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