Weather Alert in Michigan

Recent Locations: Lilliwaup, WA   Charleroi, PA   Brown City, MI  

Winter Storm Watch issued March 31 at 3:40PM EDT until April 2 at 8:00PM EDT by NWS Gaylord MI

AREAS AFFECTED: Western Chippewa; Central Chippewa; Southeast Chippewa; Western Mackinac; Eastern Mackinac; Mackinac Island/Bois Blanc Island

DESCRIPTION: * WHAT...Heavy mixed precipitation possible. Total snow and sleet accumulations between 2 and 4 inches and ice accumulations between one tenth and one quarter of an inch possible. Winds could gust 25 to 35 mph from the east. * WHERE...A portion of Eastern Upper Michigan. * WHEN...From late Wednesday night through Thursday evening. * IMPACTS...Plan on slippery road conditions. The hazardous conditions could impact the Thursday morning and evening commutes. * ADDITIONAL DETAILS...Precipitation is expected to start as snow early Thursday morning and continue through midday before transitioning to more sleet and freezing rain during the afternoon. Temperatures are expected to warm above freezing by Thursday evening.

INSTRUCTION: Monitor the latest forecasts for updates on this situation.

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North America Water Vapor (Moisture)

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Weather Topic: What are Cirrus Clouds?

Home - Education - Cloud Types - Cirrus Clouds

Cirrus Clouds Next Topic: Condensation

Cirrus clouds are high-level clouds that occur above 20,000 feet and are composed mainly of ice crystals. They are thin and wispy in appearance.

What do they indicate?
They are often the first sign of an approaching storm.

Next Topic: Condensation

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

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