Weather Alerts for Alaska
1. Blizzard Warning for: St Lawrence Island
2. High Surf Advisory for: SW Kenai Peninsula
3. Special Weather Statement for: Delta Junction; Tanana Flats; Eielson AFB and Salcha; Goldstream Valley and Nenana Hills; Fairbanks Metro Area; Nenana; Northern Denali Borough
4. Special Weather Statement for: Northern Seward Peninsula; Upper Kobuk Valleys; Shishmaref; Bering Strait Coast; Southern Seward Peninsula Coast; Interior Seward Peninsula; Lower Koyukuk Valley
5. Special Weather Statement for: South Slopes Of The Eastern Brooks Range; South Slopes Of The Central Brooks Range; Upper Koyukuk Valley; Yukon Flats
6. Special Weather Statement for: Thompson Pass
7. Wind Advisory for: Eastern Alaska Range North of Trims Camp
8. Winter Storm Warning for: Eastern Alaska Range South of Trims Camp
9. Winter Storm Warning for: Eastern Norton Sound and Nulato Hills
10. Winter Storm Warning for: Lower Yukon and Innoko Valleys; Upper Kuskokwim Valley
11. Winter Storm Warning for: Middle Yukon Valley
12. Winter Storm Warning for: Yukon Delta Coast; Lower Yukon River
13. Winter Weather Advisory for: Dalton Highway Summits
14. Winter Weather Advisory for: Northern Copper Valley; Northern Susitna Valley
15. Winter Weather Advisory for: Shishmaref; Bering Strait Coast
16. Winter Weather Advisory for: Southern Denali Borough
17. Winter Weather Advisory for: White Mountains and High Terrain South of the Yukon River; Upper Chena River Valley; Chatanika River Valley; Two Rivers; Central Interior
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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
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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