Weather Alert in Minnesota

Recent Locations: Grants Pass, OR   Waseca, MN  

Winter Storm Warning issued February 16 at 10:17PM 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 5 and 8 inches except between 8 and 11 inches for the higher terrain northeast of Duluth. Ice accumulations around one tenth of an inch. East 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 Tuesday 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 Tuesday night 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 Contrails?

Home - Education - Cloud Types - Contrails

Contrails Next Topic: Cumulonimbus Clouds

A contrail is an artificial cloud, created by the passing of an aircraft.

Contrails form because water vapor in the exhaust of aircraft engines is suspended in the air under certain temperatures and humidity conditions. These contrails are called exhaust contrails.

Another type of contrail can form due to a temporary reduction in air pressure moving over the plane's surface, causing condensation. These are called aerodynamic contrails.

When you can see your breath on a cold day, it is also because of condensation. The reason contrails last longer than the condensation from your breath is because the water in contrails freezes into ice particles.

Next Topic: Cumulonimbus Clouds

Weather Topic: What are Cumulus Clouds?

Home - Education - Cloud Types - Cumulus Clouds

Cumulus Clouds Next Topic: Drizzle

Cumulus clouds are fluffy and textured with rounded tops, and may have flat bottoms. The border of a cumulus cloud is clearly defined, and can have the appearance of cotton or cauliflower.

Cumulus clouds form at low altitudes (rarely above 2 km) but can grow very tall, becoming cumulus congestus and possibly the even taller cumulonimbus clouds. When cumulus clouds become taller, they have a greater chance of producing precipitation.

Next Topic: Drizzle

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