Weather Alert in Minnesota
Winter Weather Advisory issued February 19 at 2:19AM CST until February 19 at 8:00AM CST by NWS Twin Cities/Chanhassen MN
AREAS AFFECTED: Douglas; Stevens; Pope; Stearns; Swift; Kandiyohi; Meeker
DESCRIPTION: ...CONTINUED LIGHT SNOW TONING AND SNOW COVERED ROADS WILL LEAD TO A SLOW COMMUTE THURSDAY MORNING... .Snow will slowly diminish through the rest of tonight from Morris and Alexandria, east into the Twin Cities and far western Wisconsin. Additional snow accumulations will be up to 1 inch, though the light snow will result in continue snow covered roads in Thursday morning, which will result in a slow commute Thursday morning. * WHAT...Snow. Additional snow accumulations up to two inches. * WHERE...Kandiyohi, Meeker, Stearns, Douglas, Pope, Stevens, and Swift Counties. * WHEN...Until 8 AM CST this morning. * IMPACTS...Snow covered roads will lead to hazardous conditions impacting the Thursday morning commute.
INSTRUCTION: Slow down and use caution while traveling. Call 5 1 1 or visit 511mn.org for road conditions.
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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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