Weather Alerts for New York
1. Coastal Flood Watch for: Bronx; Northwest Suffolk; Northern Queens; Northern Nassau
2. Coastal Flood Watch for: Northeast Suffolk; Southeast Suffolk
3. Coastal Flood Watch for: Southwest Suffolk; Southern Nassau
4. Flood Watch for: Steuben
5. Flood Watch for: Tompkins
6. Special Weather Statement for: Eastern Albany; Western Rensselaer; Eastern Greene; Western Columbia; Eastern Ulster; Western Dutchess
7. Winter Storm Warning for: Hamilton; Northern Warren; Southeast Warren; Bennington; Western Windham; Eastern Windham
8. Winter Storm Warning for: Northern St. Lawrence; Eastern Clinton; Southern Franklin; Western Clinton; Western Essex; Eastern Essex; Grand Isle; Washington; Orange; Eastern Addison; Eastern Rutland; Western Windsor; Eastern Windsor
9. Winter Storm Watch for: Northwest Suffolk; Northeast Suffolk; Southwest Suffolk; Southeast Suffolk
10. Winter Weather Advisory for: Northern Franklin; Southeastern St. Lawrence; Southwestern St. Lawrence; Western Franklin; Orleans; Essex; Western Chittenden; Lamoille; Caledonia; Western Addison; Western Rutland; Eastern Franklin; Eastern Chittenden
11. Winter Weather Advisory for: Northern Herkimer; Southern Herkimer; Southern Fulton; Montgomery; Schoharie; Western Schenectady; Eastern Schenectady; Western Albany; Western Greene; Western Ulster; Northern Fulton
12. Winter Weather Advisory for: Northern Oneida
13. Winter Weather Advisory for: Oswego; Jefferson; Lewis
14. Winter Weather Advisory for: Southern Oneida; Otsego; Delaware; Sullivan
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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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