Forecast Details for Malin, OR

Recent Locations: Malin, OR  
Tonight: Clear, with a low around 31. West northwest wind around 5 mph becoming calm after midnight.
Friday: Sunny, with a high near 64. Calm wind becoming west northwest 5 to 8 mph in the afternoon.
Friday Night: Mostly clear, with a low around 33. Northwest wind 5 to 8 mph becoming calm after midnight.
Saturday: A 20 percent chance of rain after 11am. Snow level 4600 feet rising to 6300 feet in the afternoon. Mostly sunny, with a high near 61. Light north northwest wind becoming west 5 to 10 mph in the afternoon. Winds could gust as high as 20 mph.
Saturday Night: A 30 percent chance of rain before 11pm. Snow level 6400 feet lowering to 4700 feet after midnight . Partly cloudy, with a low around 32. West northwest wind 5 to 14 mph, with gusts as high as 23 mph.
Sunday: A 30 percent chance of rain after 11am. Snow level 4300 feet rising to 5400 feet in the afternoon. Mostly sunny, with a high near 57.
Sunday Night: A 30 percent chance of rain before 11pm. Snow level 5900 feet lowering to 5400 feet after midnight . Partly cloudy, with a low around 34.
Monday: A slight chance of rain. Snow level 5200 feet rising to 6100 feet in the afternoon. Mostly sunny, with a high near 59.
Monday Night: Partly cloudy, with a low around 35.
Tuesday: Sunny, with a high near 64.
Tuesday Night: Mostly clear, with a low around 35.
Wednesday: Sunny, with a high near 68.
Wednesday Night: Mostly clear, with a low around 38.
Thursday: Sunny, with a high near 70.

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Current U.S. National Radar--Current

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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

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