Weather Alert in North Carolina
High Wind Watch issued February 5 at 8:57PM EST until February 7 at 7:00PM EST by NWS Greenville-Spartanburg SC
AREAS AFFECTED: Avery; Alexander; Yancey; Mitchell; Buncombe; Southern Jackson; Transylvania; Henderson; Caldwell Mountains; Greater Caldwell; Burke Mountains; Greater Burke; McDowell Mountains; Eastern McDowell; Rutherford Mountains; Greater Rutherford; Polk Mountains; Eastern Polk; Greenville Mountains
DESCRIPTION: * WHAT...Northwest winds 20 to 30 mph with gusts up to 65 mph possible. * WHERE...Portions of western North Carolina and Upstate South Carolina. * WHEN...From Friday evening through Saturday evening. * IMPACTS...Damaging winds could blow down trees and power lines. Widespread power outages are possible. Travel could be difficult, especially for high profile vehicles. * ADDITIONAL DETAILS...The strong winds will result in cold wind chills across the mountains early Saturday morning, and some blowing snow near the Tennessee border.
INSTRUCTION: Be prepared for possible power outages. Take time now to fasten or shelter loose objects in a safe location prior to the onset of high winds. 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.
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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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