Weather Alerts for Montana
1. Avalanche Watch for: Flathead, MT
2. Avalanche Watch for: Kootenai/Cabinet Region
3. Avalanche Watch for: West Glacier Region
4. High Wind Warning for: Northern Sweet Grass; Melville Foothills
5. High Wind Watch for: Cascade County below 5000ft; Judith Basin County and Judith Gap
6. High Wind Watch for: East Glacier Park Region; Northern High Plains; Southern High Plains
7. High Wind Watch for: Eastern Glacier, Western Toole, and Central Pondera
8. High Wind Watch for: Red Lodge Foothills
9. High Wind Watch for: Southern Big Horn; Bighorn Canyon; Sheridan Foothills
10. High Wind Watch for: Southern Rocky Mountain Front
11. High Wind Watch for: Upper Blackfoot and MacDonald Pass; Gates of the Mountains; Little Belt and Highwood Mountains; Helena Valley; Big Belt, Bridger and Castle Mountains; Meagher County Valleys; Elkhorn and Boulder Mountains; Canyon Ferry Area; Missouri Headwaters; Gallatin Valley
12. Wind Advisory for: Livingston Area; Beartooth Foothills
13. Winter Storm Warning for: Absaroka/Beartooth Mountains
14. Winter Weather Advisory for: East Glacier Park Region
15. Winter Weather Advisory for: Kootenai/Cabinet Region
16. Winter Weather Advisory for: Lower Clark Fork Region
17. Winter Weather Advisory for: West Glacier Region
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Current U.S. National Radar--Current
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National Weather Forecast for Tomorrow
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North America Water Vapor (Moisture)
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Weather Topic: What is Evaporation?
Home - Education - Precipitation - Evaporation
Next Topic: Fog
Evaporation is the process which returns water from the earth
back to the atmosphere, and is another crucial process in the water cycle.
Evaporation is the transformation of liquid into gas, and it happens because
molecules are excited by the application of energy and turn into vapor.
In order for water to evaporate it has to be on the surface of a body of water.
Next Topic: Fog
Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
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