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 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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