Weather Alert in Ohio
Winter Weather Advisory issued February 6 at 12:44PM EST until February 6 at 10:00PM EST by NWS Cleveland OH
AREAS AFFECTED: Wood; Sandusky; Hancock; Seneca; Wyandot; Crawford; Marion; Morrow; Knox
DESCRIPTION: * WHAT...Snow and blowing snow expected. Additional snow accumulations up to one inch. Winds gusting as high as 40 mph. * WHERE...Portions of north central and northwest Ohio. * WHEN...Until 10 PM EST this evening. * IMPACTS...Plan on slippery conditions with with slower travel likely. Blowing snow can significantly reduce visibility this evening. The hazardous conditions could impact the evening commute. * ADDITIONAL DETAILS...After a few hours of dry weather this afternoon, snow showers, wind gusts up to 40 mph, and falling temperatures will lead to blowing and drifting snow and locally hazardous road conditions this evening.
INSTRUCTION: Slow down and use caution while traveling. The Ohio Department of Transportation and Ohio Turnpike and Infrastructure Commission strongly encourage motorists to heed all travel restrictions and delay unnecessary travel. Visit www.ohgo.com for the latest travel, roadway, and traffic conditions.
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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
Weather Topic: What are Cumulus Clouds?
Home - Education - Cloud Types - Cumulus Clouds
Next Topic: Drizzle
Cumulus clouds are fluffy and textured with rounded tops, and
may have flat bottoms. The border of a cumulus cloud
is clearly defined, and can have the appearance of cotton or cauliflower.
Cumulus clouds form at low altitudes (rarely above 2 km) but can grow very tall,
becoming cumulus congestus and possibly the even taller cumulonimbus clouds.
When cumulus clouds become taller, they have a greater chance of producing precipitation.
Next Topic: Drizzle
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