Weather Alerts for New York
1. Flood Advisory for: Warren, NY
2. Flood Warning for: Jefferson, NY; Lewis, NY
3. High Wind Warning for: Cattaraugus
4. High Wind Warning for: Chautauqua
5. High Wind Warning for: Monroe
6. High Wind Warning for: Niagara; Orleans; Northern Erie; Genesee; Wyoming; Southern Erie
7. Wind Advisory for: Onondaga; Madison; Southern Oneida; Cortland; Chenango; Otsego; Tioga; Broome; Delaware; Sullivan; Susquehanna; Northern Wayne; Lackawanna; Luzerne; Pike; Southern Wayne
8. Wind Advisory for: Wayne; Northern Cayuga; Livingston; Ontario; Allegany
9. Wind Advisory for: Yates; Seneca; Southern Cayuga; Steuben; Schuyler; Chemung; Tompkins; Bradford; Wyoming
10. Winter Storm Warning for: Northern Herkimer; Hamilton
11. Winter Storm Warning for: Northern Oneida
12. Winter Storm Warning for: Oswego; Jefferson; Lewis
13. Winter Storm Warning for: Wyoming; Cattaraugus; Southern Erie
14. Winter Weather Advisory for: Allegany
15. Winter Weather Advisory for: Chautauqua
16. Winter Weather Advisory for: Northern Warren; Northern Fulton
17. Winter Weather Advisory for: Southeastern St. Lawrence; Southern Franklin; Western Essex; Eastern Rutland; Western Windsor
18. Winter Weather Advisory for: Western Greene; Western Ulster
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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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