Weather Alerts for New Jersey
1. Coastal Flood Advisory for: Gloucester; Camden; Northwestern Burlington; Delaware; Philadelphia; Lower Bucks
2. Coastal Flood Advisory for: Hudson; Eastern Essex; Eastern Union; New York (Manhattan)
3. Coastal Flood Advisory for: Hudson; Eastern Essex; Eastern Union; New York (Manhattan)
4. Coastal Flood Warning for: Atlantic Coastal Cape May
5. Coastal Flood Warning for: Coastal Atlantic
6. Coastal Flood Warning for: Coastal Ocean
7. Coastal Flood Warning for: Cumberland
8. Coastal Flood Warning for: Eastern Monmouth
9. Coastal Flood Warning for: Middlesex; Western Monmouth
10. Coastal Flood Warning for: Ocean; Atlantic; Southeastern Burlington
11. High Surf Advisory for: Atlantic Coastal Cape May
12. High Surf Advisory for: Coastal Atlantic
13. High Surf Advisory for: Coastal Ocean
14. High Surf Advisory for: Eastern Monmouth
15. Rip Current Statement for: Atlantic Coastal Cape May
16. Rip Current Statement for: Coastal Atlantic
17. Rip Current Statement for: Coastal Ocean
18. Rip Current Statement for: Eastern Monmouth
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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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