Forecast Details for Cannonville, UT

Recent Locations: Canastota, NY Broussard, LA Cannonville, UT

Tonight: Mostly clear, with a low around 5. Wind chill values as low as -7. North northwest wind 9 to 14 mph.

Thursday: Snow likely, mainly after 2pm. Increasing clouds, with a high near 33. Wind chill values as low as -6. North northwest wind 6 to 13 mph becoming south in the morning. Chance of precipitation is 60%. New snow accumulation of less than one inch possible.

Thursday Night: Snow. Low around 14. Wind chill values as low as 3. Southwest wind 9 to 13 mph. Chance of precipitation is 100%. New snow accumulation of 3 to 7 inches possible.

Friday: A 50 percent chance of snow, mainly before 11am. Mostly sunny, with a high near 35. Wind chill values as low as 2. West northwest wind around 14 mph. New snow accumulation of less than a half inch possible.

Friday Night: Mostly clear, with a low around 5. North northwest wind around 9 mph.

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.

Tuesday Night: A slight chance of rain. Mostly cloudy, with a low around 32.

Wednesday: A chance of rain. 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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National Weather Forecast for Tomorrow

Tomorrow National Weather Forecast and Tomorrow National Weather Map are show below.

North America Water Vapor (Moisture)

This map shows recent moisture content over North America. Bright and colored areas show high moisture (ie, clouds); brown indicates very little moisture present; black indicates no moisture.

Weather Topic: What are Stratocumulus Clouds?

Home - Education - Cloud Types - Stratocumulus Clouds

Next Topic: Stratus Clouds

Stratocumulus clouds are similar to altocumulus clouds in their fluffy appearance, but have a slightly darker shade due to their additional mass.

A good way to distinguish the two cloud types is to hold your hand out and measure the size of an individual cloud; if it is the size of your thumb it is generally an altocumulus cloud, if it is the size of your hand it is generally a stratocumulus cloud.

It is uncommon for stratocumulus clouds to produce precipitation, but if they do it is usually a light rain or snow.

Next Topic: Stratus Clouds

Weather Topic: What are Wall Clouds?

Home - Education - Cloud Types - Wall Clouds

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