Weather Alert in Ohio
Severe Thunderstorm Warning issued March 26 at 9:27PM EDT until March 26 at 10:00PM EDT by NWS Pittsburgh PA
AREAS AFFECTED: Jefferson, OH; Washington, PA; Brooke, WV; Hancock, WV
DESCRIPTION: At 927 PM EDT, a severe thunderstorm was located over Steubenville, moving east at 55 mph. HAZARD...Ping pong ball size hail and 60 mph wind gusts. SOURCE...Radar indicated. IMPACT...People and animals outdoors will be injured. Expect hail damage to roofs, siding, windows, and vehicles. Expect wind damage to roofs, siding, and trees. Locations impacted include... Weirton, Steubenville, Washington, Canonsburg, Wellsburg, Avella, Cecil-Bishop, Wintersville, Mingo Junction, Follansbee, Wolfdale, McGovern, Hooverson Heights, East Washington, Houston, Bethany, Smithfield, Claysville, Franklin and Hickory.
INSTRUCTION: Seek shelter inside a well-built structure and stay away from windows. This storm is capable of producing damaging winds and 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. A Tornado Watch remains in effect until 1100 PM EDT Thursday for portions of east central Ohio, southwest Pennsylvania, and the northern panhandle of West Virginia.
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Weather Topic: What are Cirrus Clouds?
Home - Education - Cloud Types - Cirrus Clouds
Next Topic: Condensation
Cirrus clouds are high-level clouds that occur above 20,000 feet
and are composed mainly of ice crystals.
They are thin and wispy in appearance.
What do they indicate?
They are often the first sign of an approaching storm.
Next Topic: Condensation
Weather Topic: What are Contrails?
Home - Education - Cloud Types - Contrails
Next Topic: Cumulonimbus Clouds
A contrail is an artificial cloud, created by the passing of an
aircraft.
Contrails form because water vapor in the exhaust of aircraft engines is suspended
in the air under certain temperatures and humidity conditions. These contrails
are called exhaust contrails.
Another type of contrail can form due to a temporary reduction in air pressure
moving over the plane's surface, causing condensation.
These are called aerodynamic contrails.
When you can see your breath on a cold day, it is also because of condensation.
The reason contrails last longer than the condensation from your breath is
because the water in contrails freezes into ice particles.
Next Topic: Cumulonimbus Clouds
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