Weather Alert in Virginia
Special Weather Statement issued February 6 at 11:00PM EST by NWS Wakefield VA
AREAS AFFECTED: Fluvanna; Prince Edward; Cumberland; Goochland; Caroline; Mecklenburg; Lunenburg; Nottoway; Amelia; Powhatan; Charles City; New Kent; Western Louisa; Eastern Louisa; Western Hanover; Eastern Hanover; Western Chesterfield; Western Henrico (Including the City of Richmond); Eastern Henrico; Western King William; Eastern King William; Western King and Queen; Eastern King and Queen; Western Essex; Eastern Essex
DESCRIPTION: With temperatures below freezing tonight into Monday and wet, slushy, or snow-covered roads from the snow today, black ice is possible tonight into Saturday, especially on untreated, secondary, and back roads. Slow down and use caution when driving, especially when traversing roads that have not been treated.
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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