Forecast Details for Bayview, ID

Recent Locations: Florida, NY   Andrews, NC   Bayview, ID  
Overnight: A 30 percent chance of rain. Snow level 4300 feet. Mostly cloudy, with a low around 35. Calm wind. New precipitation amounts of less than a tenth of an inch possible.
Wednesday: Rain. Snow level 4600 feet rising to 5500 feet in the afternoon. High near 46. Light and variable wind. Chance of precipitation is 100%. New precipitation amounts between a tenth and quarter of an inch possible.
Wednesday Night: Rain, possibly mixed with snow before 4am, then rain between 4am and 5am, then rain, possibly mixed with snow after 5am. Snow level 5500 feet lowering to 3500 feet after midnight . Low around 35. Calm wind becoming southwest around 5 mph after midnight. Chance of precipitation is 100%. Little or no snow accumulation expected.
Thursday: Rain and snow, becoming all rain after 2pm. Snow level 2800 feet rising to 3500 feet in the afternoon. High near 42. Southwest wind 6 to 9 mph, with gusts as high as 20 mph. Chance of precipitation is 90%. Little or no snow accumulation expected.
Thursday Night: A 50 percent chance of rain before 11pm. Snow level 4400 feet lowering to 3600 feet after midnight . Mostly cloudy, with a low around 33. Southwest wind around 6 mph becoming calm in the evening. New precipitation amounts of less than a tenth of an inch possible.
Friday: Partly sunny, with a high near 49.
Friday Night: Partly cloudy, with a low around 32.
Saturday: Mostly sunny, with a high near 56.
Saturday Night: Partly cloudy, with a low around 36.
Sunday: Mostly sunny, with a high near 61.
Sunday Night: Mostly cloudy, with a low around 38.
Monday: Partly sunny, with a high near 64.
Monday Night: Mostly cloudy, with a low around 42.
Tuesday: Mostly sunny, with a high near 64.

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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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