Weather Alert in New York
Winter Weather Advisory issued February 5 at 12:44PM EST until February 8 at 7:00AM EST by NWS Buffalo NY
AREAS AFFECTED: Monroe; Wayne; Northern Cayuga; Oswego; Livingston; Ontario
DESCRIPTION: * WHAT...A combination of widespread snow and localized lake effect snow expected. Total snow accumulations 3 to 6 inches expected in most areas, with 4 to 7 inches expected along the Lake Ontario shoreline. Winds gusting as high as 35 mph will create areas of blowing and drifting snow. * WHERE...Monroe, Wayne, Northern Cayuga, Oswego, Livingston, and Ontario Counties. * WHEN...From 1 PM Friday to 7 AM EST Sunday. * IMPACTS...Travel will be difficult. The hazardous conditions may impact the Friday evening commute. * ADDITIONAL DETAILS...An Arctic front will bring widespread snow showers to the region Friday morning, which will then taper off to more localized lake effect snow Friday night through Saturday. Winds strengthening behind this front late Friday evening through Saturday will resulting of blowing and drifting of the fresh snowpack.
INSTRUCTION: Periods of snow will result in snow covered roads and limited visibilities. Slow down and use caution while driving. Submit snow reports through our website or social media. During lake effect snow, the weather can vary from bands of locally heavy snow with greatly reduced visibilities to dry conditions just a few miles away. Be prepared for rapid changes in weather, visibility, and road 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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