Weather Alert in Tennessee
Winter Weather Advisory issued February 23 at 1:22PM EST until February 24 at 12:00AM EST by NWS Morristown TN
AREAS AFFECTED: Johnson; Cocke Smoky Mountains; Southeast Greene; Unicoi; Southeast Carter; Blount Smoky Mountains; Sevier Smoky Mountains
DESCRIPTION: * WHAT...Occasional snow showers will continue through this evening. Snow accumulations of 1 to 4 inches have been reported with up to 6 inches over the highest peaks. Additional snow accumulations of 1/2 to 1 inch is expected. Northwest winds gusting to around 30 mph. Wind chill values from 5 above to 5 degrees below zero. * WHERE...Far east Tennessee mountains. * WHEN...Until midnight EST tonight. * IMPACTS...Plan on snow and ice covered road conditions. The hazardous conditions could impact the Monday morning and evening commutes. Gusty winds could bring down tree branches.
INSTRUCTION: Be prepared for slippery roads. Slow down and use caution while driving. If you are going outside, watch your first few steps taken on stairs, sidewalks, and driveways. These surfaces could be icy and slippery, increasing your risk of a fall and injury.
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Weather Topic: What are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
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
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