Weather Alert in Ohio

Recent Locations: Cleveland, OH   Columbus, OH   Cincinnati, OH  

Severe Thunderstorm Warning issued March 26 at 9:05PM EDT until March 26 at 9:45PM EDT by NWS Pittsburgh PA

AREAS AFFECTED: Coshocton, OH; Guernsey, OH; Muskingum, OH; Tuscarawas, OH

DESCRIPTION: SVRPBZ The National Weather Service in Pittsburgh has issued a * Severe Thunderstorm Warning for... Coshocton County in east central Ohio... Northwestern Guernsey County in east central Ohio... Northeastern Muskingum County in east central Ohio... Southwestern Tuscarawas County in east central Ohio... * Until 945 PM EDT. * At 905 PM EDT, a severe thunderstorm was located 25 miles northwest of Frazeysburg, or 30 miles northwest of Coshocton, moving east at 65 mph. HAZARD...60 mph wind gusts and half dollar size hail. SOURCE...Radar indicated. IMPACT...Hail damage to vehicles is expected. Expect wind damage to roofs, siding, and trees. * Locations impacted include... Coshocton, Newcomerstown, West Lafayette, Dresden, Warsaw, Port Washington, Conesville, Plainfield, Nellie, Otsego, Chili, Blissfield, Cooperdale, Layland, Boden, Bakersville, New Guilford and Walhonding.

INSTRUCTION: Seek shelter inside a well-built structure and stay away from windows. This storm is capable of producing damaging winds and large hail. Tornadoes can develop quickly from severe thunderstorms. Seek shelter immediately in an interior room on the lowest floor of a well-built structure. A Tornado Watch remains in effect until 1100 PM EDT Thursday for a portion of east central Ohio.

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Weather Topic: What are Altocumulus Clouds?

Home - Education - Cloud Types - Altocumulus Clouds

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

Weather Topic: What are Cirrocumulus Clouds?

Home - Education - Cloud Types - Cirrocumulus Clouds

Cirrocumulus Clouds Next Topic: Cirrostratus Clouds

Cirrocumulus clouds form at high altitudes (usually around 5 km) and have distinguishing characteristics displayed in a fine layer of small cloud patches. These small cloud patches are sometimes referred to as "cloudlets" in relation to the whole cloud formation.

Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the water droplets in the cloud freeze into ice crystals and the cloud becomes a cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud formations generally pass rapidly.

Next Topic: Cirrostratus Clouds

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