Forecast Details for Clyde Park, MT

Recent Locations: Clyde Park, MT  
Current Alerts for Clyde Park, MT: Hydrologic Outlook
Today: A 50 percent chance of rain after noon. Mostly cloudy, with a high near 46. Light and variable wind becoming east 8 to 13 mph in the morning.
Tonight: Rain and snow likely before midnight, then a slight chance of snow. Mostly cloudy, with a low around 27. East southeast wind 6 to 13 mph becoming west southwest in the evening. Chance of precipitation is 60%. New snow accumulation of less than one inch possible.
Monday: Mostly sunny, with a high near 52. West southwest wind 11 to 16 mph increasing to 18 to 23 mph in the afternoon.
Monday Night: Mostly cloudy, with a low around 28. Southwest wind 20 to 24 mph.
Tuesday: Partly sunny, with a high near 53. South southwest wind 18 to 24 mph.
Tuesday Night: A 30 percent chance of snow showers after midnight. Mostly cloudy, with a low around 29. Little or no snow accumulation expected.
Wednesday: A chance of snow showers before noon, then rain showers likely. Mostly cloudy, with a high near 46. Chance of precipitation is 60%. New snow accumulation of less than a half inch possible.
Wednesday Night: Rain and snow showers likely, becoming all snow after midnight. Cloudy, with a low around 26. Chance of precipitation is 70%.
Thursday: Snow likely before noon, then rain and snow likely. Cloudy, with a high near 38. Chance of precipitation is 70%.
Thursday Night: A 50 percent chance of snow. Mostly cloudy, with a low around 18.
Friday: A 30 percent chance of snow. Mostly cloudy, with a high near 36.
Friday Night: Partly cloudy, with a low around 16.
Saturday: Mostly sunny, with a high near 39.

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Weather Topic: What are Shelf Clouds?

Home - Education - Cloud Types - Shelf Clouds

shelf clouds Next Topic: Wall Clouds

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: Wall Clouds

Weather Topic: What is Condensation?

Home - Education - Precipitation - Condensation

condensation Next Topic: Drizzle

Condensation is the process which creates clouds, and therefore it is a crucial process in the water cycle. Condensation is the change of matter from a state of gas into a state of liquid, and it happens because water molecules release heat into the atmosphere and become organized into a more closely packed structure, what we might see as water droplets.

Water is always present in the air around us as a vapor, but it's too small for us to see. When water undergoes the process of condensation it becomes organized into visible water droplets. You've probably seen condensation happen before on the surface of a cold drink!

Next Topic: Drizzle