Weather Alert in West Virginia

Recent Locations: Bealeton, VA   Colchester, VT   Kegley, WV  

Winter Storm Warning issued March 2 at 8:43AM EST until March 3 at 10:00AM EST by NWS Charleston WV

AREAS AFFECTED: Northwest Pocahontas; Southeast Randolph

DESCRIPTION: * WHAT...Heavy mixed precipitation. Total snow accumulations between 1 and 3 inches and ice accumulations around three tenths of an inch. Locally higher amounts of ice accumulations could be possible. * WHERE...Northwest Pocahontas and Southeast Randolph Counties. * WHEN...Until 10 AM EST Tuesday. * IMPACTS...Power outages and tree damage are likely due to the ice. Travel could be nearly impossible. The hazardous conditions could impact the Monday evening and Tuesday morning commutes.

INSTRUCTION: If you must travel, keep an extra flashlight, food, and water in your vehicle in case of an emergency. The latest road conditions for the state you are calling from can be obtained by calling 5 1 1 or by accessing the online traffic and roadway portal for your state. Additional information can be found at https://www.weather.gov/rlx as well as on our X and Facebook pages.

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Current U.S. National Radar--Current

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North America Water Vapor (Moisture)

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Weather Topic: What are Cirrus Clouds?

Home - Education - Cloud Types - Cirrus Clouds

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

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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