Weather Alert in Ohio

Recent Locations: Evansville, IN   Columbus, OH   Yonkers, NY  

Severe Thunderstorm Warning issued March 22 at 10:05PM EDT until March 22 at 10:30PM EDT by NWS Pittsburgh PA

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

DESCRIPTION: At 1005 PM EDT, a severe thunderstorm was located 9 miles north of Dresden, or 9 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, 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. Continuous cloud to ground lightning is occurring with this storm. Lightning is one of nature's leading killers. Remember, if you can hear thunder, you are close enough to be struck by lightning.

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Weather Topic: What is Evaporation?

Home - Education - Precipitation - Evaporation

Evaporation Next Topic: Fog

Evaporation is the process which returns water from the earth back to the atmosphere, and is another crucial process in the water cycle.

Evaporation is the transformation of liquid into gas, and it happens because molecules are excited by the application of energy and turn into vapor. In order for water to evaporate it has to be on the surface of a body of water.

Next Topic: Fog

Weather Topic: What are Fractus Clouds?

Home - Education - Cloud Types - Fractus Clouds

Fractus Clouds Next Topic: Freezing Rain

A fractus cloud (scud) is a fragmented, tattered cloud which has likely been sheared off of another cloud. They are accessory clouds, meaning they develop from parent clouds, and are named in a way which describes the original cloud which contained them.

Fractus clouds which have originated from cumulus clouds are referred to as cumulus fractus, while fractus clouds which have originated from stratus clouds are referred to as stratus fractus. Under certain conditions a fractus cloud might merge with another cloud, or develop into a cumulus cloud, but usually a fractus cloud seen by itself will dissipate rapidly.

They are often observed on the leading and trailing edges of storm clouds, and are a display of wind activity.

Next Topic: Freezing Rain

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