Weather Alert in Kentucky
Special Weather Statement issued March 2 at 2:25AM EST by NWS Jackson KY
AREAS AFFECTED: Montgomery; Estill; Powell; Menifee; Morgan; Johnson; Wolfe; Magoffin; Lee; Martin
DESCRIPTION: A system moving into the area may bring a wintry mix of precipitation during the morning commute until a few hours after sunrise today. Precipitation may start as snow, but quickly transition to a mix. A light coating of snow cannot be ruled out, but a light glaze of ice may develop on untreated bridges, overpasses, and other elevated surfaces. Thus, a few slick or icy spots are possible during the morning commute. Motorists are encouraged to slow down and allow plenty of extra time to reach your destination Monday morning.
INSTRUCTION: N/A
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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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