Weather Alert in Minnesota
Winter Storm Warning issued February 17 at 1:00PM CST until February 19 at 12:00PM CST by NWS Duluth MN
AREAS AFFECTED: Central St. Louis; Carlton/South St. Louis
DESCRIPTION: * WHAT...Heavy snow with light ice accumulations expected. Total snow accumulations between 4 and 8 inches except between 8 and 12 inches for the higher terrain northeast of Duluth. Ice accumulations up to one tenth of an inch. Winds gusting as high as 55 mph. * WHERE...Carlton and South and Central St. Louis Counties. This includes the Tribal Lands of the Fond du Lac Band and the Bois Forte Band, Lake Vermilion area. * WHEN...From 6 PM this evening to noon CST Thursday. * IMPACTS...The strong winds and weight of snow on tree limbs may down power lines and could cause sporadic power outages. Travel could be very difficult. The hazardous conditions could impact the Wednesday morning and evening commutes. * ADDITIONAL DETAILS...The strongest winds are expected Tuesday evening through Wednesday morning from the east off Lake Superior. Near whiteout conditions are possible for a few hour period late this evening through very early Wednesday morning as high snowfall rates could combine with those peak winds gusting to 55 mph.
INSTRUCTION: If you must travel, keep an extra flashlight, food, and water in your vehicle in case of an emergency. Call 511 or visit www.511mn.org for Minnesota road information. Do not touch downed lines and report any power outages to your electric company. Slick roadways and the possibility of downed trees and power lines may create hazardous travel 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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