Weather Alert in Kentucky
Special Weather Statement issued March 23 at 2:56AM EDT by NWS Jackson KY
AREAS AFFECTED: Morgan; Johnson; Magoffin
DESCRIPTION: At 256 AM EDT, Doppler radar was tracking a strong thunderstorm over Ezel, or 9 miles west of West Liberty, moving east at 50 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... West Liberty, Salyersville, Mason, Henry, Lewis, Zag, Moon, Florress, Lick Branch, Pekin, Falcon, Omer, Wonnie, Burning Fork, Kernie, West Royalton Station, Panama, Ezel, Gillem Branch, and Redbush. THIS INCLUDES Bert T. Combs Mountain Parkway between mile markers 62 and 76.
INSTRUCTION: If outdoors, consider seeking shelter inside a building.
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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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