Forecast Details for Logan, UT

Recent Locations: Metamora, MI   Gardiner, OR   Logan, UT  
Today: Rain and snow showers, becoming all snow after noon. Some thunder is also possible. High near 46. South southwest wind 7 to 10 mph becoming west in the afternoon. Chance of precipitation is 100%. Little or no snow accumulation expected.
Tonight: A 40 percent chance of snow showers before midnight. Mostly cloudy, with a low around 26. West wind 5 to 10 mph becoming light and variable after midnight. New snow accumulation of less than a half inch possible.
Friday: Partly sunny, with a high near 48. Light and variable wind.
Friday Night: Mostly clear, with a low around 27. West southwest wind around 5 mph becoming calm in the evening.
Saturday: Sunny, with a high near 60. Calm wind.
Saturday Night: Mostly clear, with a low around 32.
Sunday: Sunny, with a high near 65.
Sunday Night: Mostly clear, with a low around 37.
Monday: Sunny, with a high near 68.
Monday Night: Partly cloudy, with a low around 40.
Tuesday: A slight chance of showers and thunderstorms. Mostly sunny, with a high near 70.
Tuesday Night: Partly cloudy, with a low around 42.
Wednesday: A chance of showers and thunderstorms. Partly sunny, with a high near 67.

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Current U.S. National Radar--Current

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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

Weather Topic: What are Altostratus Clouds?

Home - Education - Cloud Types - Altostratus Clouds

Altostratus Clouds Next Topic: Cirrocumulus Clouds

Altostratus clouds form at mid to high-level altitudes (between 2 and 7 km) and are created by a warm, stable air mass which causes water vapor to condense as it rise through the atmosphere. Usually altostratus clouds are featureless sheets characterized by a uniform color.

In some cases, wind punching through the cloud formation may give it a waved appearance, called altostratus undulatus. Altostratus clouds are commonly seen with other cloud formations accompanying them.

Next Topic: Cirrocumulus Clouds

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