Weather Alerts for New York
1. Extreme Heat Watch for: Eastern Clinton; Grand Isle; Western Franklin; Western Chittenden
2. Extreme Heat Watch for: Eastern Essex; Western Addison; Eastern Windsor
3. Extreme Heat Watch for: New York (Manhattan); Bronx; Richmond (Staten Is.); Kings (Brooklyn); Northern Queens; Southern Queens
4. Extreme Heat Watch for: Northern Saratoga; Eastern Schenectady; Southern Saratoga; Eastern Albany; Western Rensselaer; Eastern Greene; Western Columbia; Eastern Columbia; Southeast Warren; Southern Washington
5. Extreme Heat Watch for: Northern Washington; Eastern Windham
6. Heat Advisory for: Eastern Essex; Western Addison; Eastern Windsor
7. Heat Advisory for: Jefferson; Lewis
8. Heat Advisory for: Monroe; Wayne; Northern Cayuga; Oswego; Livingston; Ontario
9. Heat Advisory for: Niagara; Orleans; Northern Erie; Genesee; Wyoming; Chautauqua; Cattaraugus; Allegany; Southern Erie
10. Heat Advisory for: Northern Oneida; Yates; Seneca; Southern Cayuga; Steuben; Madison; Southern Oneida; Cortland; Chenango; Otsego; Delaware
11. Heat Advisory for: Northern Saratoga; Eastern Schenectady; Southern Saratoga; Eastern Albany; Western Rensselaer; Eastern Greene; Western Columbia; Eastern Columbia; Southeast Warren; Southern Washington
12. Heat Advisory for: Northern St. Lawrence; Southwestern St. Lawrence; Western Rutland
13. Heat Advisory for: Northern Washington; Eastern Windham
14. Heat Advisory for: Onondaga; Schuyler; Chemung; Tompkins; Tioga; Broome; Sullivan; Bradford; Susquehanna; Northern Wayne; Wyoming; Lackawanna; Luzerne; Pike; Southern Wayne
15. Heat Advisory for: Southern Herkimer; Southern Fulton; Montgomery; Western Schenectady
16. Heat Advisory for: Southern Herkimer; Southern Fulton; Montgomery; Western Schenectady
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National Weather Forecast for Tomorrow
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North America Water Vapor (Moisture)
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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
Weather Topic: What are Altostratus Clouds?
Home - Education - Cloud Types - Altostratus Clouds
Next Topic: Cirrocumulus Clouds
Altostratus clouds form at mid to high-level altitudes
(between 2 and 7 km) and are created by a warm, stable air mass which causes
water vapor
to condense as it rise through the atmosphere. Usually altostratus clouds are
featureless sheets characterized by a uniform color.
In some cases, wind punching through the cloud formation may give it a waved
appearance, called altostratus undulatus. Altostratus clouds
are commonly seen with other cloud formations accompanying them.
Next Topic: Cirrocumulus Clouds
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