Weather Alerts for New York
1. Beach Hazards Statement for: Monroe
2. Beach Hazards Statement for: Niagara; Orleans
3. Coastal Flood Advisory for: Kings (Brooklyn)
4. Coastal Flood Advisory for: Kings (Brooklyn)
5. Coastal Flood Advisory for: Northeast Suffolk
6. Coastal Flood Advisory for: Southeast Suffolk
7. Coastal Flood Advisory for: Southern Queens
8. Coastal Flood Advisory for: Southern Queens
9. Coastal Flood Advisory for: Southwest Suffolk; Southern Nassau
10. Coastal Flood Advisory for: Southwest Suffolk; Southern Nassau
11. Coastal Flood Warning for: Northeast Suffolk
12. Coastal Flood Warning for: Southeast Suffolk
13. Coastal Flood Warning for: Southern Queens
14. Coastal Flood Warning for: Southwest Suffolk; Southern Nassau
15. High Surf Advisory for: Kings (Brooklyn)
16. High Surf Advisory for: Southeast Suffolk
17. High Surf Advisory for: Southern Queens
18. High Surf Advisory for: Southwest Suffolk; Southern Nassau
19. Rip Current Statement for: Kings (Brooklyn)
20. Rip Current Statement for: Southeast Suffolk
21. Rip Current Statement for: Southern Queens
22. Rip Current Statement for: Southwest Suffolk; Southern Nassau
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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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