Forecast Details for Cannonville, UT

Recent Locations: Fond du Lac, WI   Cordova, MD   Cannonville, UT  
This Afternoon: Snow likely, mainly before 2pm. Partly sunny, with a high near 35. Windy, with a west wind 25 to 30 mph, with gusts as high as 47 mph. Chance of precipitation is 70%. Total daytime snow accumulation of 3 to 5 inches possible.
Tonight: Mostly clear, with a low around 5. Wind chill values as low as -7. Northwest wind 15 to 20 mph decreasing to 9 to 14 mph in the evening. Winds could gust as high as 33 mph.
Thursday: A 40 percent chance of snow after 11am. Increasing clouds, with a high near 33. Wind chill values as low as -5. North northwest wind 6 to 11 mph becoming south in the morning. New snow accumulation of less than one inch possible.
Thursday Night: Snow. Low around 16. Wind chill values as low as 7. Southwest wind 10 to 14 mph. Chance of precipitation is 90%. New snow accumulation of 3 to 5 inches possible.
Friday: Snow likely, mainly before 11am. Partly sunny, with a high near 34. West northwest wind around 15 mph. Chance of precipitation is 60%. New snow accumulation of less than a half inch possible.
Friday Night: Mostly clear, with a low around 5.
Saturday: Sunny, with a high near 37.
Saturday Night: Mostly cloudy, with a low around 16.
Sunday: Mostly sunny, with a high near 44.
Sunday Night: Partly cloudy, with a low around 21.
Monday: Partly sunny, with a high near 50.
Monday Night: Mostly cloudy, with a low around 28.
Tuesday: Partly sunny, with a high near 53.

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Current U.S. National Radar--Current

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National Weather Forecast--Current

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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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