Weather Alert in West Virginia
Special Weather Statement issued February 8 at 8:04PM EST by NWS Charleston WV
AREAS AFFECTED: Northwest Pocahontas; Southeast Pocahontas; Northwest Randolph; Southeast Randolph
DESCRIPTION: High pressure with clear, calm conditions atop the snowpack provide the perfect mid-winter setup for a frigid night and early Monday morning. Temperatures will bottom out in the single digits, single digits below zero in the normally colder low spots away from rivers, even isolated double digit lows below zero in the normally coldest sheltered mountain valleys, particularly for northern portions of Randolph and Pocahontas counties. Even with little or no wind, these low temperatures can lead to frostbite in as little as 30 minutes on exposed skin, as well as hypothermia. Bundle up if you must venture outside anytime tonight through early Monday morning, including the morning commute and bus run. If traveling, be prepared in case of a breakdown.
INSTRUCTION: N/A
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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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