Weather Alert in North Carolina
Winter Weather Advisory issued February 5 at 1:25AM EST until February 5 at 10:00AM EST by NWS Raleigh NC
AREAS AFFECTED: Person; Granville; Vance; Warren; Halifax; Forsyth; Guilford; Alamance; Orange; Durham; Franklin; Nash; Edgecombe; Davidson; Randolph; Chatham; Wake; Johnston; Wilson; Lee; Harnett; Wayne; Cumberland; Sampson
DESCRIPTION: * WHAT...Mixed precipitation. Additional snow accumulations of a dusting to locally a half inch of snow, and ice accumulations around a light glaze. * WHERE...A portion of central North Carolina. * WHEN...Until 10 AM EST this morning. * IMPACTS...Plan on slippery road conditions. The hazardous conditions could impact the Thursday morning commute.
INSTRUCTION: Slow down and use caution while traveling. The latest road conditions for the state you are calling from can be obtained by calling 5 1 1.
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North America Water Vapor (Moisture)
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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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