Forecast Details for Manchester, VT

Recent Locations: Nemacolin, PA   Clinton, NC   Manchester, VT  
Tonight: Mostly cloudy, with a low around 28. Light south wind.
Tuesday: A chance of rain showers, snow showers, and freezing rain before 9am, then a slight chance of rain and snow showers between 9am and noon. Mostly cloudy, with a high near 39. Southwest wind 3 to 5 mph. Chance of precipitation is 30%. New snow accumulation of less than a half inch possible.
Tuesday Night: Mostly cloudy, with a low around 27. Light southwest wind.
Wednesday: A chance of snow before 10am, then rain and snow. High near 36. Light and variable wind. Chance of precipitation is 90%. New snow accumulation of less than one inch possible.
Wednesday Night: Snow, possibly mixed with rain before 1am, then a chance of snow. Low around 18. Light north wind. Chance of precipitation is 80%. New precipitation amounts between a tenth and quarter of an inch possible.
Thursday: Mostly sunny, with a high near 35.
Thursday Night: Partly cloudy, with a low around 18.
Friday: Snow likely, mainly after 1pm. Mostly cloudy, with a high near 36. Chance of precipitation is 70%.
Friday Night: Snow likely, mainly before 1am. Mostly cloudy, with a low around 25. Chance of precipitation is 70%.
Saturday: A chance of snow. Mostly cloudy, with a high near 35. Chance of precipitation is 50%.
Saturday Night: A chance of snow. Mostly cloudy, with a low around 19. Chance of precipitation is 30%.
Sunday: A chance of snow. Partly sunny, with a high near 33. Chance of precipitation is 30%.
Sunday Night: A chance of snow. Mostly cloudy, with a low around 18. Chance of precipitation is 40%.
Monday: A chance of snow. Partly sunny, with a high near 31. Chance of precipitation is 30%.

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Current U.S. National Radar--Current

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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

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