Weather Alert in North Dakota
Winter Weather Advisory issued February 18 at 4:38AM CST until February 19 at 12:00AM CST by NWS Bismarck ND
AREAS AFFECTED: Burleigh; Kidder; Stutsman; Sioux; Emmons; Logan; La Moure; McIntosh; Dickey
DESCRIPTION: * WHAT...Snow. Total snow accumulations between 1 and 4 inches. Winds gusting as high as 50 mph. * WHERE...South central North Dakota. * WHEN...Until midnight CST /11 PM MST/ tonight. * IMPACTS...Travel could become difficult. Widespread blowing snow could significantly reduce visibility. The hazardous conditions will impact the morning and evening commutes. * ADDITIONAL DETAILS...Near blizzard conditions at times, especially in open country.
INSTRUCTION: Slow down and use caution while traveling. The latest road conditions can be obtained by calling 5 1 1.
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North America Water Vapor (Moisture)
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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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