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 is Graupel?
Home - Education - Precipitation - Graupel
Next Topic: Hail
Graupel is a form of precipitation that is created by atmospheric conditions
which cause supercooled water droplets to contact snow crystals and freeze to
their surface.
Sometimes known as soft hail or snow pellets, graupel is delicate and easily
destroyed by touch. Whereas hail usually falls during severe weather, graupel
doesn't require such conditions to form, and can form in mild precipitation
similar to situations which produce snowfall.
Next Topic: Hail
Weather Topic: What are Hole Punch Clouds?
Home - Education - Cloud Types - Hole Punch Clouds
Next Topic: Mammatus Clouds
A hole punch cloud is an unusual occurrence when a disk-shaped
hole appears in a cirrostratus, cirrocumulus, or altocumulus cloud.
When part of the cloud forms ice crystals, water droplets in the surrounding area
of the cloud evaporate. The effect of this process produces a large elliptical
gap in the cloud. The hole punch cloud formation is rare, but it is not specific
to any geographic area.
Other names which have been used to describe this phenomena include fallstreak hole,
skypunch, and cloud hole.
Next Topic: Mammatus Clouds
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