Weather Alerts for South Dakota
1. Blizzard Warning for: Codington; Grant; Hamlin; Deuel
2. Blizzard Warning for: Faulk; Spink; Clark; Hyde; Hand
3. Blizzard Warning for: McPherson; Brown; Edmunds
4. Blizzard Warning for: Stanley; Hughes; Jones; Lyman; Buffalo
5. Winter Storm Warning for: Butte; Northern Meade Co Plains; Haakon; Sturgis/Piedmont Foothills; Southern Meade Co Plains; Northeastern Crook
6. Winter Storm Warning for: Codington; Grant; Hamlin; Deuel
7. Winter Storm Warning for: Corson; Campbell; Walworth; Dewey; Potter; Sully
8. Winter Storm Warning for: Faulk; Spink; Clark; Hyde; Hand
9. Winter Storm Warning for: Harding; Northern Perkins; Southern Perkins
10. Winter Storm Warning for: McPherson; Brown; Edmunds
11. Winter Storm Warning for: Northern Black Hills; Northern Foothills; Wyoming Black Hills
12. Winter Storm Warning for: Ziebach
13. Winter Storm Watch for: Beadle; Kingsbury; Jerauld; Sanborn; Miner; Lake
14. Winter Storm Watch for: Brule; Aurora; Davison; Hanson; McCook; Douglas; Hutchinson
15. Winter Storm Watch for: Gregory; Charles Mix
16. Winter Weather Advisory for: Rapid City; Pennington Co Plains; Northern Oglala Lakota; Northern Jackson; Bennett; Mellette; Todd; Tripp; Southern Oglala Lakota; Southern Jackson
17. Winter Weather Advisory for: Stanley; Hughes; Jones; Lyman; Buffalo
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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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