Weather Alert in Ohio
Severe Thunderstorm Warning issued April 29 at 4:29PM EDT until April 29 at 5:15PM EDT by NWS Cleveland OH
AREAS AFFECTED: Cuyahoga, OH; Geauga, OH; Mahoning, OH; Portage, OH; Stark, OH; Summit, OH; Trumbull, OH
DESCRIPTION: SVRCLE The National Weather Service in Cleveland has issued a * Severe Thunderstorm Warning for... Trumbull County in northeastern Ohio... Mahoning County in northeastern Ohio... Portage County in northeastern Ohio... Southern Geauga County in northeastern Ohio... Southeastern Cuyahoga County in northeastern Ohio... Stark County in northeastern Ohio... Summit County in northeastern Ohio... * Until 515 PM EDT. * At 429 PM EDT, severe thunderstorms were located along a line extending from 6 miles northwest of Cuyahoga Falls to near Waynesburg, moving northeast at 50 mph. HAZARD...60 mph wind gusts and penny size hail. SOURCE...Radar indicated. IMPACT...Expect damage to trees and power lines. * Locations impacted include... Akron, Canton, Youngstown, Warren, Salem, Ravenna, Columbiana, Cuyahoga Falls, Boardman, North Royalton, Kent, Barberton, Green, Solon, Alliance, Hudson, Niles, Twinsburg, Tallmadge, and North Canton.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building.
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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
Weather Topic: What are Altostratus Clouds?
Home - Education - Cloud Types - Altostratus Clouds
Next Topic: Cirrocumulus Clouds
Altostratus clouds form at mid to high-level altitudes
(between 2 and 7 km) and are created by a warm, stable air mass which causes
water vapor
to condense as it rise through the atmosphere. Usually altostratus clouds are
featureless sheets characterized by a uniform color.
In some cases, wind punching through the cloud formation may give it a waved
appearance, called altostratus undulatus. Altostratus clouds
are commonly seen with other cloud formations accompanying them.
Next Topic: Cirrocumulus Clouds
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