Weather Alert in New York
Special Weather Statement issued September 3 at 3:13PM EDT by NWS Albany NY
AREAS AFFECTED: Northern Saratoga; Northern Warren; Northern Washington; Western Schenectady; Eastern Schenectady; Southern Saratoga; Western Albany; Eastern Albany; Western Rensselaer; Eastern Rensselaer; Eastern Greene; Western Columbia; Eastern Columbia; Eastern Ulster; Western Dutchess; Eastern Dutchess; Southeast Warren; Southern Washington
DESCRIPTION: The combination of recent dry weather and increasing drought, southerly winds gusting between 25 and 35 mph and relative humidity values between 35 and 40 percent will contribute to an elevated risk for fire spread tomorrow. The risk will be greatest across portions of the Hudson Valley Fire Danger Rating Area which includes the following counties: Warren, Saratoga, Washington, Schenectady, Albany, Rensselaer, Columbia, Dutchess, eastern Greene and eastern Ulster counties. Any fires that develop in these areas could spread rapidly. Residents are encouraged to exercise caution if handling any potential ignition sources, such as machinery, cigarettes, or matches. For more information about wildfire danger and wildfire prevention, please visit the New York Department of Environmental Conservation website at http://dec.ny.gov/environmental- protection/wildfires.
INSTRUCTION: N/A
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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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