Weather Alerts for Alaska
1. Special Weather Statement for: Lower Yukon River; Lower Yukon and Innoko Valleys; North Slopes of the Western Alaska Range; Upper Kuskokwim Valley
2. Special Weather Statement for: Northern Seward Peninsula; Southern Seward Peninsula Coast; Interior Seward Peninsula
3. Special Weather Statement for: Upper Kobuk Valleys; Lower Koyukuk Valley
4. Winter Storm Warning for: Kuskokwim Delta Coast and Nunivak Island
5. Winter Storm Warning for: Yukon Delta Coast
6. Winter Storm Watch for: Eastern Norton Sound and Nulato Hills
7. Winter Storm Watch for: Middle Yukon Valley
8. Winter Storm Watch for: St Lawrence Island
9. Winter Weather Advisory for: Eastern Alaska Range South of Trims Camp
10. Winter Weather Advisory for: Kuskokwim Valley West; Kuskokwim Valley East; Lime Village; Interior Kuskokwim Delta
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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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