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