Weather Alerts for New York
Winter Weather Advisory
1. Cold Weather Advisory for: Eastern Clinton; Eastern Essex; Grand Isle; Western Franklin; Orleans; Essex; Western Chittenden; Lamoille; Caledonia; Washington; Western Addison; Orange; Western Rutland; Eastern Franklin; Eastern Chittenden; Eastern Addison; Eastern Rutland; Western Windsor; Eastern Windsor
2. Cold Weather Advisory for: Niagara; Orleans; Monroe; Wayne; Northern Cayuga; Northern Erie; Genesee
3. Cold Weather Advisory for: Northern Saratoga; Northern Washington; Eastern Schenectady; Southern Saratoga; Eastern Albany; Western Rensselaer; Eastern Greene; Western Columbia; Southeast Warren; Southern Washington; Eastern Windham
4. Extreme Cold Warning for: Northern Herkimer; Hamilton; Southern Herkimer; Southern Fulton; Montgomery; Schoharie; Western Schenectady; Western Albany; Western Greene; Western Ulster; Northern Fulton
5. Extreme Cold Warning for: Northern Oneida; Yates; Seneca; Southern Cayuga; Onondaga; Steuben; Schuyler; Chemung; Tompkins; Madison; Southern Oneida; Cortland; Chenango; Tioga; Broome; Bradford; Susquehanna; Wyoming; Lackawanna; Luzerne
6. Extreme Cold Warning for: Northern St. Lawrence; Northern Franklin; Southeastern St. Lawrence; Southern Franklin; Western Clinton; Western Essex; Southwestern St. Lawrence
7. Extreme Cold Warning for: Northern Warren
8. Extreme Cold Warning for: Oswego; Jefferson; Lewis
9. Extreme Cold Warning for: Otsego; Delaware; Sullivan; Northern Wayne; Pike; Southern Wayne
10. Extreme Cold Warning for: Wyoming; Livingston; Ontario; Chautauqua; Cattaraugus; Allegany; Southern Erie
11. Winter Weather Advisory for: Eastern Rensselaer; Bennington
12. Winter Weather Advisory for: Monroe; Wayne; Northern Cayuga; Oswego; Livingston; Ontario
13. Winter Weather Advisory for: Niagara; Orleans; Northern Erie; Genesee; Wyoming; Chautauqua; Cattaraugus; Southern Erie
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North America Water Vapor (Moisture)
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Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
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