Weather Alert in Ohio

Recent Locations: New Albany, OH  
Current Alerts for New Albany, OH: Heat Advisory

Severe Thunderstorm Warning issued July 28 at 5:06PM EDT until July 28 at 6:00PM EDT by NWS Cleveland OH

AREAS AFFECTED: Erie, OH; Lorain, OH

DESCRIPTION: SVRCLE The National Weather Service in Cleveland has issued a * Severe Thunderstorm Warning for... Erie County in north central Ohio... Central Lorain County in north central Ohio... * Until 600 PM EDT. * At 506 PM EDT, a severe thunderstorm was located near Western Vermilion, moving east at 20 mph. HAZARD...60 mph wind gusts and penny size hail. SOURCE...Radar indicated. IMPACT...Expect damage to trees and power lines. * Locations impacted include... Lorain, Elyria, Western Vermilion, Vermilion, North Ridgeville, Avon Lake, Amherst, Grafton, Northern Milan, Avon, Bay Village, Sheffield Lake, Oberlin, Sheffield, Lagrange, South Amherst, Pittsfield, Berlin Heights, Kipton, and Birmingham.

INSTRUCTION: For your protection move to an interior room on the lowest floor of a building. Torrential rainfall is occurring with this storm, and may lead to flash flooding. Do not drive your vehicle through flooded roadways.

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Weather Topic: What are Wall Clouds?

Home - Education - Cloud Types - Wall Clouds

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

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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