Weather Alert in Ohio
Severe Thunderstorm Warning issued April 29 at 4:10PM EDT until April 29 at 4:30PM EDT by NWS Pittsburgh PA
AREAS AFFECTED: Belmont, OH; Carroll, OH; Guernsey, OH; Harrison, OH; Tuscarawas, OH
DESCRIPTION: At 409 PM EDT, severe thunderstorms were located along a line extending from near East Sparta to 6 miles northwest of Freeport to near Byesville, moving east at 60 mph. THESE ARE DESTRUCTIVE STORMS FOR southern Tuscarawas and Harrison Counties. HAZARD...80 mph wind gusts. SOURCE...Radar indicated. IMPACT...Extensive tree damage and widespread power outages. Mobile homes will be heavily damaged. Expect considerable damage to roofs, windows and vehicles. Locations impacted include... New Philadelphia, Dover, Cambridge, Uhrichsville, Barnesville, Carrollton, Freeport, Minerva, Dennison, Strasburg, Byesville, Gnadenhutten, Antrim, Malvern, Tuscarawas, Bolivar, Flushing, Scio, Midvale, and Mineral City.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building. Please report severe weather by calling 412-262-1988, posting to the NWS Pittsburgh Facebook page, or using X @NWSPITTSBURGH.
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Weather Topic: What are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
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
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