Weather Alert in Virginia
Winter Weather Advisory issued February 21 at 1:59PM EST until February 24 at 1:00AM EST by NWS Blacksburg VA
AREAS AFFECTED: Bland; Giles; Bath; Monroe; Eastern Greenbrier
DESCRIPTION: Low pressure will pass over the region tonight and Sunday with rain changing to snow across the higher elevations. Arrival of colder air Sunday along with the development of a strong winter storm along the coastal mid-atlantic will result in an extended period of snow across the mountains Sunday night through Monday. * WHAT...Snow expected. Total snow accumulations up to 3 inches. Winds gusting as high as 40 mph. * WHERE...In Virginia, Bland, Giles, and Bath Counties. In West Virginia, Eastern Greenbrier and Monroe Counties. * WHEN...From 1 AM Sunday to 1 AM EST Tuesday. * IMPACTS...Plan on slippery road conditions. The hazardous conditions could impact the Monday morning and evening commutes. * ADDITIONAL DETAILS...Temperatures are expected to fall into the teens Sunday night with wind chills in the single digits.
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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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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