Forecast Details for Tokio, ND

Recent Locations: Amory, MS   Big Flat, AR   Tokio, ND  
Overnight: Mostly cloudy, with a low around 21. East wind around 9 mph.
Wednesday: A 30 percent chance of snow after 1pm. Mostly cloudy, with a high near 34. Breezy, with an east southeast wind 14 to 20 mph. Little or no snow accumulation expected.
Wednesday Night: A chance of snow before 2am, then a chance of snow after 3am. Cloudy, with a low around 27. East southeast wind 14 to 17 mph. Chance of precipitation is 40%. New snow accumulation of less than one inch possible.
Thursday: Snow likely, mainly after 7am. Mostly cloudy, with a high near 33. East wind 16 to 18 mph. Chance of precipitation is 60%.
Thursday Night: A 50 percent chance of snow. Cloudy, with a low around 27. Northeast wind 11 to 17 mph.
Friday: Snow likely, mainly after 1pm. Cloudy, with a high near 33. Northeast wind 13 to 17 mph. Chance of precipitation is 60%.
Friday Night: Snow. Low around 27. North wind around 15 mph. Chance of precipitation is 80%.
Saturday: A 40 percent chance of snow before 1pm. Partly sunny, with a high near 33. Breezy, with a north northwest wind 17 to 21 mph.
Saturday Night: Partly cloudy, with a low around 19. West northwest wind 10 to 17 mph.
Sunday: Mostly sunny, with a high near 37. Southwest wind 8 to 13 mph.
Sunday Night: A 20 percent chance of snow. Mostly cloudy, with a low around 26. West southwest wind around 11 mph becoming north after midnight.
Monday: A 20 percent chance of snow. Mostly cloudy, with a high near 34. North wind 13 to 15 mph.
Monday Night: Mostly cloudy, with a low around 18. North wind 8 to 10 mph becoming south southeast after midnight.
Tuesday: Partly sunny, with a high near 35. South southeast wind 10 to 18 mph.

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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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