Forecast Details for Broadbent, OR

Recent Locations: Broadbent, OR  
Overnight: Cloudy, with a low around 40. Light southeast wind.
Friday: A 20 percent chance of showers. Snow level 2900 feet rising to 3900 feet in the afternoon. Mostly cloudy, with a high near 61. Calm wind becoming north northeast around 6 mph in the afternoon.
Friday Night: Mostly cloudy, then gradually becoming mostly clear, with a low around 39. North wind around 6 mph becoming calm in the evening.
Saturday: Sunny, with a high near 65. Light north wind increasing to 5 to 10 mph in the afternoon.
Saturday Night: Partly cloudy, with a low around 42. North wind 6 to 13 mph, with gusts as high as 20 mph.
Sunday: Mostly sunny, with a high near 62.
Sunday Night: Mostly clear, with a low around 41.
Monday: Sunny, with a high near 68.
Monday Night: Mostly clear, with a low around 44.
Tuesday: Mostly sunny, with a high near 71.
Tuesday Night: Mostly cloudy, with a low around 44.
Wednesday: A chance of showers. Partly sunny, with a high near 56.
Wednesday Night: A chance of showers. Snow level 3500 feet lowering to 2300 feet after midnight . Mostly cloudy, with a low around 39.
Thursday: Showers likely. Snow level 2200 feet. Mostly cloudy, with a high near 54.

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Current U.S. National Radar--Current

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Current U.S. National Radar

National Weather Forecast--Current

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Today's National Weather Map

National Weather Forecast for Tomorrow

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Tomorrows National Weather Map

North America Water Vapor (Moisture)

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North American Water Vapor Map

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