Weather Alert in Ohio

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Severe Thunderstorm Warning issued March 22 at 9:52PM EDT until March 22 at 10:30PM 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 1030 PM EDT. * At 952 PM EDT, a severe thunderstorm was located 14 miles northwest of Frazeysburg, or 22 miles west of Coshocton, moving east at 60 mph. HAZARD...Half dollar size hail. SOURCE...Radar indicated. IMPACT...Damage to vehicles is expected. * Locations impacted include... Coshocton, Newcomerstown, West Lafayette, Warsaw, Conesville, Plainfield, Nellie, Otsego, Gilmore, Boden, Cooperdale, New Guilford, Walhonding, Birmingham, Kimbolton and Salt Fork State Park.

INSTRUCTION: Seek shelter inside a well-built structure and stay away from windows. This storm is capable of producing large hail.

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Weather Topic: What is Snow?

Home - Education - Precipitation - Snow

Snow Next Topic: Stratocumulus Clouds

Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake, has unique characteristics, but all of them grow in a hexagonal structure. Snowfall can last for sustained periods of time and result in significant buildup of snow on the ground.

On the earth's surface, snow starts out light and powdery, but as it begins to melt it tends to become more granular, producing small bits of ice which have the consistency of sand. After several cycles of melting and freezing, snow can become very dense and ice-like, commonly known as snow pack.

Next Topic: Stratocumulus Clouds

Weather Topic: What are Stratus Clouds?

Home - Education - Cloud Types - Stratus Clouds

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.

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