Weather Alert in North Carolina
Special Weather Statement issued March 22 at 2:15PM EDT by NWS Raleigh NC
AREAS AFFECTED: Person; Granville; Vance; Warren; Forsyth; Guilford; Alamance; Orange; Durham; Franklin; Davidson; Randolph; Chatham; Wake; Stanly; Montgomery; Moore; Lee; Harnett; Anson; Richmond; Scotland; Hoke; Cumberland
DESCRIPTION: The combination of dry fine fuels, relative humidities around 25 to 30 percent, northerly wind gusts around 20 to 25 mph, and warm temperatures will lead to an increased risk for the rapid spread of wildfires on Monday across the Piedmont and Sandhills of central North Carolina. Residents and visitors are urged to properly dispose of cigarette butts, matches, and any other flammable items in appropriate containers. Additionally, exercise caution if operating any equipment that could create sparks and keep vehicles off of dry grass. Most dry grasses, dead leaves, and other tree litter could easily ignite and spread fire quickly. Lastly, remember to obey local burn bans. For more information about wildfire danger, burn restrictions, and wildfire prevention and education, please visit the North Carolina forestry or environmental protection website.
INSTRUCTION: N/A
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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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