Weather Alert in Kentucky
Special Weather Statement issued February 23 at 3:10AM EST by NWS Jackson KY
AREAS AFFECTED: Fleming; Montgomery; Bath; Rowan; Estill; Powell; Menifee; Rockcastle; Jackson; Pulaski; Laurel; Wayne; McCreary; Whitley; Knox; Elliott; Morgan; Johnson; Wolfe; Magoffin; Lee; Breathitt; Owsley; Clay
DESCRIPTION: Some light snow accumulations will continue today as rounds of snow showers track across the area. Wind gusts as high as 30 mph could occur in the heavier snow showers. This, when combined with the falling snow, could produce sudden sharp visibility reductions and quick light snow accumulations, especially on this afternoon. Expect event total snow accumulations between a dusting and around 1 inch, with locally higher amounts possible wherever snow showers are the most persistent today. Temperatures this morning will be in the low to mid 20s, so expect times of slick, slushy, or snow covered roads. Any untreated roads and surfaces, including bridges, overpasses, decks, and steps may be icy. If traveling today, slow down and exercise caution. Allow plenty of extra time to reach your destination.
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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