Forecast Details for Cazenovia, WI

Recent Locations: Saint Donatus, IA Cazenovia, WI

Overnight: Patchy fog after 5am. Otherwise, mostly cloudy, with a steady temperature around 65. Light east wind.

Sunday: Patchy fog before 9am. Otherwise, partly sunny, then gradually becoming sunny, with a high near 85. East wind 3 to 7 mph.

Sunday Night: Mostly clear, with a low around 61. Southeast wind 3 to 6 mph.

Monday: Mostly sunny, with a high near 85. South wind 3 to 8 mph.

Monday Night: Partly cloudy, with a low around 62. Southeast wind around 5 mph becoming calm after midnight.

Tuesday: Mostly sunny, with a high near 86. Calm wind becoming south around 6 mph in the afternoon.

Tuesday Night: Partly cloudy, with a low around 62. Calm wind.

Wednesday: A slight chance of showers, with thunderstorms also possible after 1pm. Mostly sunny, with a high near 84. Calm wind becoming south around 6 mph in the afternoon. Chance of precipitation is 20%.

Wednesday Night: A 30 percent chance of showers and thunderstorms. Mostly cloudy, with a low around 60. Calm wind.

Thursday: A chance of showers, with thunderstorms also possible after 1pm. Mostly cloudy, with a high near 79. Calm wind becoming south around 6 mph in the afternoon. Chance of precipitation is 30%.

Thursday Night: A 40 percent chance of showers and thunderstorms. Mostly cloudy, with a low around 59. East wind 3 to 5 mph.

Friday: A 30 percent chance of showers and thunderstorms. Mostly cloudy, with a high near 75. East wind 5 to 9 mph.

Friday Night: A 20 percent chance of showers. Mostly cloudy, with a low around 56. Northeast wind 6 to 8 mph.

Saturday: A 20 percent chance of showers. Partly sunny, with a high near 70. East wind 6 to 9 mph.

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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

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North America Water Vapor (Moisture)

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Weather Topic: What are Shelf Clouds?

Home - Education - Cloud Types - Shelf Clouds

Shelf Clouds Next Topic: Sleet

A shelf cloud is similar to a wall cloud, but forms at the front of a storm cloud, instead of at the rear, where wall clouds form.

A shelf cloud is caused by a series of events set into motion by the advancing storm; first, cool air settles along the ground where precipitation has just fallen. As the cool air is brought in, the warmer air is displaced, and rises above it, because it is less dense. When the warmer air reaches the bottom of the storm cloud, it begins to cool again, and the resulting condensation is a visible shelf cloud.

Next Topic: Sleet

Weather Topic: What is Snow?

Home - Education - Precipitation - Snow

Snow Next Topic: Stratocumulus Clouds

Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake, has unique characteristics, but all of them grow in a hexagonal structure. Snowfall can last for sustained periods of time and result in significant buildup of snow on the ground.

On the earth's surface, snow starts out light and powdery, but as it begins to melt it tends to become more granular, producing small bits of ice which have the consistency of sand. After several cycles of melting and freezing, snow can become very dense and ice-like, commonly known as snow pack.

Next Topic: Stratocumulus Clouds