Weather Alerts for Alaska
1. Blizzard Warning for: Kivalina and Red Dog Dock; Baldwin Peninsula
2. Blizzard Warning for: Western Arctic Coast
3. High Wind Watch for: Kodiak Island Northeast
4. High Wind Watch for: Thompson Pass
5. Special Weather Statement for: Northern Bristol Bay Coast
6. Wind Advisory for: Municipality of Skagway
7. Wind Advisory for: Southern Kenai Mtns; West Prince William Sound & Whittier
8. Wind Advisory for: Valdez
9. Winter Storm Warning for: Interior Seward Peninsula; Eastern Norton Sound and Nulato Hills
10. Winter Storm Warning for: Noatak Valley; Lower Kobuk Valley
11. Winter Storm Warning for: Northern Denali Borough
12. Winter Storm Warning for: South Slopes of the Western Brooks Range; Upper Kobuk Valleys
13. Winter Storm Warning for: Tanana Flats; Eielson AFB and Salcha
14. Winter Storm Warning for: Upper Koyukuk Valley
15. Winter Storm Warning for: White Mountains and High Terrain South of the Yukon River; Upper Chena River Valley; Goldstream Valley and Nenana Hills; Chatanika River Valley; Two Rivers; Fairbanks Metro Area; Nenana; Central Interior
16. Winter Weather Advisory for: Central Brooks Range
17. Winter Weather Advisory for: Lower Koyukuk Valley; Middle Yukon Valley
18. Winter Weather Advisory for: Lower Yukon River
19. Winter Weather Advisory for: Northern Seward Peninsula
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North America Water Vapor (Moisture)
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Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
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