Weather Alert in North Carolina

Current Alerts for Oxford, NC: Wind Advisory

High Wind Warning issued February 6 at 1:08PM EST until February 7 at 7:00PM EST by NWS Greenville-Spartanburg SC

AREAS AFFECTED: Avery

DESCRIPTION: * WHAT...For the High Wind Warning, northwest winds 25 to 35 mph with gusts up to 55 to 60 mph, with 75 mph gusts on ridgetops expected. For the Cold Weather Advisory, very cold wind chills as low as 10 below expected. * WHERE...Avery County. * WHEN...For the High Wind Warning, from 7 PM this evening to 7 PM EST Saturday. For the Cold Weather Advisory, from 1 AM Saturday to 7 AM EST Sunday. * IMPACTS...Damaging winds will blow down trees and power lines. Widespread power outages are expected. Travel will be difficult, especially for high profile vehicles. The dangerously cold wind chills as low as 20 below zero could result in hypothermia or frostbite if precautions are not taken. * ADDITIONAL DETAILS...A Winter Weather Advisory is also in effect for Avery County for snow accumulation through 7 am Saturday. Expect difficult travel on snow covered roads. The strong winds will result in areas of blowing snow that will sharply reduce the visibility.

INSTRUCTION: Avoid being outside near trees. If caught outside, watch for falling debris or tree limbs. Remain in the lower levels of your home during the windstorm and avoid windows and overhanging trees. Use caution if you must drive. Stay tuned to NOAA Weather Radio or your favorite source of weather information for the latest updates. Additional details can be found at www.weather.gov/gsp. Use caution while traveling outside. Wear appropriate clothing, a hat, and gloves.

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Weather Topic: What are Shelf Clouds?

Home - Education - Cloud Types - Shelf Clouds

Shelf Clouds Next Topic: Sleet

A shelf cloud is similar to a wall cloud, but forms at the front of a storm cloud, instead of at the rear, where wall clouds form.

A shelf cloud is caused by a series of events set into motion by the advancing storm; first, cool air settles along the ground where precipitation has just fallen. As the cool air is brought in, the warmer air is displaced, and rises above it, because it is less dense. When the warmer air reaches the bottom of the storm cloud, it begins to cool again, and the resulting condensation is a visible shelf cloud.

Next Topic: Sleet

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

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