Weather Alert in Virginia
Special Weather Statement issued August 13 at 1:35PM EDT by NWS Wakefield VA
AREAS AFFECTED: Goochland; Caroline; Powhatan; Eastern Louisa; Western Hanover; Eastern Hanover; Western Chesterfield; Western Henrico (Including the City of Richmond); Eastern Henrico; Western King William
DESCRIPTION: At 135 PM EDT, Doppler radar was tracking a strong thunderstorm over Tuckahoe, moving north at 20 mph. HAZARD...Wind gusts up to 40 mph and heavy rain. SOURCE...Radar indicated. IMPACT...Gusty winds could knock down tree limbs and blow around unsecured objects. Reduced visibility and minor flooding possible. This strong thunderstorm will be near... Tuckahoe, Laurel, and Wyndham around 140 PM EDT. Glen Allen around 145 PM EDT. Ashland around 200 PM EDT. Randolph Macon College around 205 PM EDT. Other locations impacted by this storm include Orchid, Crozier, Vontay, Maidens, Gum Tree, Irwin, Johnsons Springs, Elmont, Etna Mills, and Gilman.
INSTRUCTION: If outdoors, consider seeking shelter inside a building.
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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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