Weather Alert in North Carolina
Winter Storm Warning issued February 21 at 1:50PM EST until February 24 at 12:00AM EST by NWS Greenville-Spartanburg SC
AREAS AFFECTED: Avery
DESCRIPTION: * WHAT...Heavy snow expected. Total snow accumulations mostly between 2 and 6 inches, with amounts up to 10 inches possible along the Tennessee border and in the high elevations. * WHERE...Avery County. * WHEN...From midnight tonight to midnight EST Monday Night. * IMPACTS...The heavy snow will make many roads impassable and may produce a few power outages due to the weight of the snow on tree limbs and power lines. The hazardous conditions could impact the Monday morning and evening commutes. * ADDITIONAL DETAILS...Winds gusting as high as 50 mph could result in areas of blowing snow and very low visibility Sunday night and Monday.
INSTRUCTION: Monitor the latest forecasts for updates on this situation. Slow down and use caution while traveling. If you must travel, keep an extra flashlight, food, and water in your vehicle in case of an emergency.
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Weather Topic: What is Evaporation?
Home - Education - Precipitation - Evaporation
Next Topic: Fog
Evaporation is the process which returns water from the earth
back to the atmosphere, and is another crucial process in the water cycle.
Evaporation is the transformation of liquid into gas, and it happens because
molecules are excited by the application of energy and turn into vapor.
In order for water to evaporate it has to be on the surface of a body of water.
Next Topic: Fog
Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
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