Weather Alert in Minnesota
Winter Weather Advisory issued March 31 at 2:50PM CDT until April 2 at 7:00PM CDT by NWS Twin Cities/Chanhassen MN
AREAS AFFECTED: Douglas; Todd; Morrison; Mille Lacs; Kanabec; Stevens; Pope; Stearns; Benton; Lac Qui Parle; Swift; Chippewa; Kandiyohi; Meeker; Yellow Medicine
DESCRIPTION: ...MESSY SPRING SYSTEM TO BRING RAIN, FREEZING RAIN, SLEET, AND SNOW TO PORTIONS OF MINNESOTA AND WISCONSIN WEDNESDAY THROUGH THURSDAY... .A strong system is expected to bring a variety of precipitation types to the region Wednesday through Thursday. While there is still some uncertainty in the exact track of the low, a mix of snow and sleet is expected for much of central and western Minnesota. Further to the south and east, sleet and freezing rain will be the primary precipitation type. Some shifts in the track are still anticipated, which will influence the total accumulations of snow, sleet, freezing rain, and rain. * WHAT...Mixed precipitation expected. Total snow accumulations between 3 and 5 inches, sleet accumulations around three quarters of an inch, and ice accumulations around one tenth of an inch. * WHERE...Benton, Kandiyohi, Meeker, Morrison, Stearns, Todd, Kanabec, Mille Lacs, Chippewa, Douglas, Lac Qui Parle, Pope, Stevens, Swift, and Yellow Medicine Counties. * WHEN...From 1 PM Wednesday to 7 PM CDT Thursday. * IMPACTS...Plan on slippery road conditions. The hazardous conditions will impact the Wednesday evening and Thursday morning commutes.
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 Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
Weather Topic: What are Altostratus Clouds?
Home - Education - Cloud Types - Altostratus Clouds
Next Topic: Cirrocumulus Clouds
Altostratus clouds form at mid to high-level altitudes
(between 2 and 7 km) and are created by a warm, stable air mass which causes
water vapor
to condense as it rise through the atmosphere. Usually altostratus clouds are
featureless sheets characterized by a uniform color.
In some cases, wind punching through the cloud formation may give it a waved
appearance, called altostratus undulatus. Altostratus clouds
are commonly seen with other cloud formations accompanying them.
Next Topic: Cirrocumulus Clouds
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