Weather Alert in Minnesota

Recent Locations: Shingleton, MI   Sears, MI   Mapleton, MN  

Winter Weather Advisory issued April 2 at 4:05PM CDT until April 4 at 7:00PM CDT by NWS Twin Cities/Chanhassen MN

AREAS AFFECTED: Douglas; Stevens; Pope

DESCRIPTION: ...FIRST ROUND OF WINTRY PRECIPITATION IS WRAPPING UP, ANOTHER ROUND OF FREEZING RAIN AND SNOW IS EXPECTED FOR TOMORROW... .A Winter Weather Advisory for western and central Minnesota goes into effect Friday for our next wintry system. Portions of western Minnesota will see a round of freezing rain and sleet early Friday with accumulations of up to two tenths of an inch. Further north, precipitation will start out as a wintry mix before transitioning to all snow late Friday. Snowfall totals of 3 to 5 inches are expected with around a tenth of an inch of ice accumulation. East central Minnesota will see 2 to 4 inches of snow along with ice accumulations up to two tenths of an inch. * WHAT...Mixed precipitation expected. Total snow accumulations between 3 and 5 inches, sleet accumulations between one tenth and two tenths of an inch, and ice accumulations up to one tenth of an inch. * WHERE...Douglas, Pope, and Stevens Counties. * WHEN...From 7 AM Friday to 7 PM CDT Saturday. * IMPACTS...Plan on slippery road conditions. The hazardous conditions will impact the Friday morning and evening 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 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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