Weather Alerts for Idaho
1. Avalanche Warning for: Bear River Range
2. Wind Advisory for: Shoshone/Lava Beds; Lower Snake River Plain; Eastern Magic Valley; Southern Hills/Albion Mountains; Raft River Region
3. Winter Storm Warning for: Bear River Range
4. Winter Weather Advisory for: Bear Lake Valley; Blackfoot Mountains; Caribou Range; Big Hole Mountains; Centennial Mountains/Island Park; Beaverhead/Lemhi Highlands
5. Winter Weather Advisory for: Central Panhandle Mountains
6. Winter Weather Advisory for: Coeur d'Alene Area; Idaho Palouse; Washington Palouse; Spokane Area
7. Winter Weather Advisory for: Lewis and Southern Nez Perce Counties
8. Winter Weather Advisory for: Lewiston Area; Lower Garfield and Asotin Counties
9. Winter Weather Advisory for: Lower Hells Canyon/Salmon River Region
10. Winter Weather Advisory for: Marsh and Arbon Highlands; Franklin/Eastern Oneida Region; Teton Valley
11. Winter Weather Advisory for: Northern Clearwater Mountains
12. Winter Weather Advisory for: Northern Panhandle
13. Winter Weather Advisory for: Orofino/Grangeville Region
14. Winter Weather Advisory for: Southern Clearwater Mountains
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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 Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
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