Weather Alert in New York
Winter Weather Advisory issued February 22 at 12:08AM EST until February 23 at 7:00PM EST by NWS Binghamton NY
AREAS AFFECTED: Madison; Chenango; Broome; Bradford
DESCRIPTION: * WHAT...Snow expected. Total snow accumulations between 2 and 7 inches. Winds gusting as high as 35 mph. * WHERE...In New York, Broome, Chenango, and Madison Counties. In Pennsylvania, Bradford County. * WHEN...From 1 PM Sunday to 7 PM EST Monday. * IMPACTS...Travel could be very difficult. The hazardous conditions could impact the Monday morning and evening commutes. * ADDITIONAL DETAILS...Gusty north-northwest winds increase overnight Sunday and persist into Monday morning, which could reduce visibilities due to blowing and drifting snow. Winds gusting as high as 35 mph possible through the day on Monday.
INSTRUCTION: Slow down and use caution while traveling. In New York, The latest road conditions for the state you are calling from can be obtained by calling 5 1 1. In Pennsylvania, The Pennsylvania Department of Transportation and Pennsylvania Turnpike Commission remind motorist to adjust speeds based on driving conditions as winter weather impacts Pennsylvania roadways. Visit www.511pa.com for the latest travel, roadways, and traffic conditions.
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Weather Topic: What are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
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
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