Weather Alerts for Michigan
1. Flood Warning for: Arenac, MI
2. Flood Warning for: Wexford, MI
3. Flood Watch for: Newaygo
4. Flood Watch for: Newaygo
5. Ice Storm Warning for: Western Chippewa; Central Chippewa; Southeast Chippewa; Western Mackinac; Eastern Mackinac; Mackinac Island/Bois Blanc Island
6. Severe Thunderstorm Warning for: Allegan, MI; Barry, MI
7. Tornado Warning for: Kalamazoo, MI; Van Buren, MI
8. Tornado Watch for: Allegan, MI; Barry, MI; Calhoun, MI; Eaton, MI; Kalamazoo, MI; Van Buren, MI
9. Winter Storm Warning for: Alger; Delta; Southern Schoolcraft; Northern Schoolcraft
10. Winter Storm Warning for: Baraga; Marquette
11. Winter Storm Warning for: Gogebic; Iron; Dickinson
12. Winter Storm Warning for: Keweenaw; Ontonagon; Houghton; Southern Houghton
13. Winter Storm Warning for: Luce
14. Winter Storm Warning for: Menominee
15. Winter Storm Watch for: Alger; Delta; Southern Schoolcraft; Northern Schoolcraft
16. Winter Storm Watch for: Baraga; Marquette
17. Winter Storm Watch for: Gogebic; Iron; Dickinson
18. Winter Storm Watch for: Keweenaw; Ontonagon; Houghton; Southern Houghton
19. Winter Storm Watch for: Luce
20. Winter Storm Watch for: Menominee
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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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