Weather Alert in New York
Winter Weather Advisory issued March 5 at 1:09AM EST until March 6 at 12:00PM EST by NWS Binghamton NY
AREAS AFFECTED: Northern Oneida; Southern Oneida; Otsego; Delaware; Sullivan
DESCRIPTION: * WHAT...Freezing rain expected. Total ice accumulations around one tenth to one quarter of an inch with slightly higher amounts in higher elevations of the Catskills. * WHERE...Delaware, Northern Oneida, Otsego, Southern Oneida, and Sullivan Counties. * WHEN...From 5 PM this afternoon to noon EST Friday. * IMPACTS...Difficult travel conditions are possible. The hazardous conditions could impact the Thursday evening and Friday morning commutes. * ADDITIONAL DETAILS...Colder air will filter in early Thursday evening with rain changing to freezing rain. Precipitation will taper off Friday morning. The highest ice amounts will be across the Catskills in the eastern portions of Delaware and Sullivan counties.
INSTRUCTION: Slow down and use caution while traveling. Prepare for possible power outages. The latest road conditions for the state you are calling from can be obtained by calling 5 1 1.
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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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