Weather Alert in Minnesota
Winter Weather Advisory issued February 27 at 9:41PM CST until February 28 at 5:00PM CST by NWS Twin Cities/Chanhassen MN
AREAS AFFECTED: Stevens; Lac Qui Parle; Swift; Chippewa; Kandiyohi; Meeker; Yellow Medicine; Renville; McLeod; Sibley; Redwood; Brown; Nicollet
DESCRIPTION: ...BAND OF HEAVY SNOW SATURDAY ALONG THE MINNESOTA RIVER VALLEY... .A quick hitting band of heavy snow is expected Saturday morning through the afternoon. Amounts will generally be on the order of 2 to 4 inches, but a narrow band of higher amounts (up to 6 inches) will likely set up somewhere within the advisory area. Snowfall rates may approach one inch per hour, which will lead to visibility reductions and hazardous travel. Snow will gradually end from west to east by Saturday evening. * WHAT...Snow expected. Total snow accumulations between 2 and 4 inches, with a band of 3 to 5 inches along the Minnesota River. * WHERE...Kandiyohi, McLeod, Meeker, Renville, Sibley, Brown, Nicollet, Redwood, Chippewa, Lac Qui Parle, Stevens, Swift, and Yellow Medicine Counties. * WHEN...From 3 AM to 5 PM CST Saturday. * IMPACTS...Plan on slippery road conditions.
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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