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 Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
Next Topic: Sleet
Weather Topic: What is Snow?
Home - Education - Precipitation - Snow
Next Topic: Stratocumulus Clouds
Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake,
has unique characteristics, but all of them grow in a hexagonal structure.
Snowfall can last for sustained periods of time and result in significant buildup
of snow on the ground.
On the earth's surface, snow starts out light and powdery, but as it begins to melt
it tends to become more granular, producing small bits of ice which have the consistency of
sand. After several cycles of melting and freezing, snow can become very dense
and ice-like, commonly known as snow pack.
Next Topic: Stratocumulus Clouds
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