Forecast Details for Tuckasegee, NC

Recent Locations: Tuckasegee, NC  
Overnight: Clear, with a low around 39. North wind 5 to 7 mph.
Wednesday: Sunny, with a high near 62. North wind around 5 mph becoming calm in the morning.
Wednesday Night: Partly cloudy, with a low around 38. Calm wind.
Thursday: A 20 percent chance of rain after 2pm. Partly sunny, with a high near 51. Light southeast wind.
Thursday Night: Rain likely, mainly after midnight. Cloudy, with a low around 39. Calm wind becoming east around 5 mph after midnight. Chance of precipitation is 70%.
Friday: Rain. High near 48. Chance of precipitation is 90%.
Friday Night: Rain likely, mainly before 7pm. Mostly cloudy, with a low around 42. Chance of precipitation is 60%.
Saturday: A chance of rain before noon, then a chance of showers after noon. Mostly cloudy, with a high near 52. Chance of precipitation is 40%.
Saturday Night: A 30 percent chance of rain before midnight. Mostly cloudy, with a low around 41.
Sunday: A 30 percent chance of rain before 9am. Mostly sunny, with a high near 55.
Sunday Night: A 40 percent chance of rain. Mostly cloudy, with a low around 39.
Monday: A 30 percent chance of showers. Mostly sunny, with a high near 50.
Monday Night: Partly cloudy, with a low around 37.
Tuesday: Sunny, with a high near 54.

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Weather Topic: What are Mammatus Clouds?

Home - Education - Cloud Types - Mammatus Clouds

mammatus clouds Next Topic: Shelf Clouds

A mammatus cloud is a cloud with a unique feature which resembles a web of pouches hanging along the base of the cloud.

In the United States, mammatus clouds tend to form in the warmer months, commonly in the Midwest and eastern regions.

While they usually form at the bottom of a cumulonimbis cloud, they can also form under altostratus, altocumulus, stratocumulus, and cirrus clouds. Mammatus clouds warn that severe weather is close.

Next Topic: Shelf Clouds

Weather Topic: What are Wall Clouds?

Home - Education - Cloud Types - Wall Clouds

wall clouds Next Topic: Condensation

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: Condensation