Weather Alert in North Carolina
Wind Advisory issued February 6 at 12:56AM EST until February 7 at 7:00PM EST by NWS Greenville-Spartanburg SC
AREAS AFFECTED: Alexander; Greater Caldwell; Greater Burke; Eastern McDowell; Greater Rutherford; Eastern Polk; Greenville Mountains
DESCRIPTION: * WHAT...Northwest winds 10 to 20 mph with gusts of up to 50 mph expected. * WHERE...In North Carolina, Alexander, Eastern McDowell, Eastern Polk, Greater Burke, Greater Caldwell, and Greater Rutherford Counties. In South Carolina, the mountains of Greenville County. * WHEN...From 7 PM this evening to 7 PM EST Saturday. * IMPACTS...Gusty winds will blow around unsecured objects. Tree limbs could be blown down and a few power outages may result.
INSTRUCTION: Winds this strong can make driving difficult, especially for high profile vehicles. Use extra caution. 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 are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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