Weather Alert in Ohio
Severe Thunderstorm Warning issued April 29 at 2:26PM EDT until April 29 at 3:15PM EDT by NWS Wilmington OH
AREAS AFFECTED: Clinton, OH; Fayette, OH; Pickaway, OH; Ross, OH
DESCRIPTION: SVRILN The National Weather Service in Wilmington has issued a * Severe Thunderstorm Warning for... Southern Fayette County in central Ohio... Northeastern Clinton County in southwestern Ohio... Southern Pickaway County in central Ohio... Northern Ross County in south central Ohio... * Until 315 PM EDT. * At 226 PM EDT, a severe thunderstorm was located over Sabina, moving east at 45 mph. HAZARD...60 mph wind gusts and penny size hail. SOURCE...Radar indicated. IMPACT...Expect damage to trees and power lines. * Locations impacted include... Deer Creek Lake, East Ringgold, New Vienna, Good Hope, Kingston, Austin, Sabina, Circleville, Lees Creek, Rock Mills, Williamsport, New Holland, Washington Court House, New Martinsburg, Pancoastburg, Plano, Aw Marion State Park, Clarksburg, Staunton, and Andersonville.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building. To report severe weather, go to our website at weather.gov/iln and submit your report via social media, when you can do so safely.
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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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