Forecast Details for Wimbledon, ND

Overnight: Mostly cloudy, with a low around 37. Light southwest wind.
Thursday: Showers, mainly before 3pm. High near 56. Breezy, with a south wind 7 to 12 mph becoming west northwest 19 to 29 mph in the afternoon. Winds could gust as high as 44 mph. Chance of precipitation is 80%. New precipitation amounts between a tenth and quarter of an inch possible.
Thursday Night: Showers likely, mainly before 1am. Mostly cloudy, with a low around 42. Windy, with a northwest wind 25 to 30 mph decreasing to 16 to 21 mph after midnight. Winds could gust as high as 45 mph. Chance of precipitation is 60%. New precipitation amounts of less than a tenth of an inch possible.
Friday: Cloudy, then gradually becoming mostly sunny, with a high near 55. Breezy, with a northwest wind 16 to 20 mph, with gusts as high as 30 mph.
Friday Night: Partly cloudy, with a low around 40. Northwest wind 9 to 15 mph.
Saturday: Mostly sunny, with a high near 58. North northwest wind 10 to 14 mph.
Saturday Night: Mostly clear, with a low around 37. North northwest wind 5 to 10 mph becoming light after midnight.
Sunday: Sunny, with a high near 64. Calm wind becoming south southwest 5 to 8 mph in the morning.
Sunday Night: Mostly clear, with a low around 45. South wind 6 to 10 mph.
Monday: Mostly sunny, with a high near 73. South wind 10 to 13 mph.
Monday Night: Mostly clear, with a low around 53. South southeast wind around 9 mph.
Tuesday: Mostly sunny, with a high near 75. East wind 7 to 11 mph.
Tuesday Night: Partly cloudy, with a low around 54. East wind around 9 mph.
Wednesday: Partly sunny, with a high near 75. East southeast wind 9 to 15 mph.

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North America Water Vapor (Moisture)

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Weather Topic: What is Condensation?

Home - Education - Precipitation - Condensation

Condensation Next Topic: Contrails

Condensation is the process which creates clouds, and therefore it is a crucial process in the water cycle. Condensation is the change of matter from a state of gas into a state of liquid, and it happens because water molecules release heat into the atmosphere and become organized into a more closely packed structure, what we might see as water droplets.

Water is always present in the air around us as a vapor, but it's too small for us to see. When water undergoes the process of condensation it becomes organized into visible water droplets. You've probably seen condensation happen before on the surface of a cold drink!

Next Topic: Contrails

Weather Topic: What are Cumulonimbus Clouds?

Home - Education - Cloud Types - Cumulonimbus Clouds

Cumulonimbus Clouds Next Topic: Cumulus Clouds

The final form taken by a growing cumulus cloud is the cumulonimbus cloud, which is very tall and dense. The tower of a cumulonimbus cloud can soar 23 km into the atmosphere, although most commonly they stop growing at an altitude of 6 km.

Even small cumulonimbus clouds appear very large in comparison to other cloud types. They can signal the approach of stormy weather, such as thunderstorms or blizzards.

Next Topic: Cumulus Clouds

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