Weather Alert in North Carolina
Cold Weather Advisory issued February 6 at 9:08PM EST until February 8 at 7:00AM EST by NWS Greenville-Spartanburg SC
AREAS AFFECTED: Yancey; Mitchell
DESCRIPTION: * WHAT...For the High Wind Warning, northwest winds 20 to 30 mph with gusts up to 55 to 60 mph, and up to 75 mph on ridgetops expected. For the Cold Weather Advisory above 3500 feet, very cold wind chills as low as 10 below expected. * WHERE...Mitchell and Yancey Counties. * WHEN...For the High Wind Warning, until 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 cause frostbite on exposed skin in as little as 30 minutes. * ADDITIONAL DETAILS...A Winter Weather Advisory is also in effect for Mitchell and Yancey counties 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 is Condensation?
Home - Education - Precipitation - Condensation
Next Topic: Contrails
Condensation is the process which creates clouds, and therefore
it is a crucial process in the water cycle.
Condensation is the change of matter from a state of gas into a state of liquid,
and it happens because water molecules release heat into the atmosphere and
become organized into a more closely packed structure, what we might see as
water droplets.
Water is always present in the air around us as a vapor, but it's too small for
us to see. When water undergoes the process of condensation it becomes organized
into visible water droplets. You've probably seen condensation happen before on the
surface of a cold drink!
Next Topic: Contrails
Weather Topic: What are Cumulonimbus Clouds?
Home - Education - Cloud Types - Cumulonimbus Clouds
Next Topic: Cumulus Clouds
The final form taken by a growing cumulus cloud is the
cumulonimbus cloud, which is very tall and dense.
The tower of a cumulonimbus cloud can soar 23 km into the atmosphere, although
most commonly they stop growing at an altitude of 6 km.
Even small cumulonimbus clouds appear very large in comparison to other cloud types.
They can signal the approach of stormy weather, such as thunderstorms or blizzards.
Next Topic: Cumulus Clouds
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