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 Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
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
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