Weather Alert in New York
Winter Weather Advisory issued March 3 at 12:06AM EST until March 4 at 3:00AM EST by NWS Albany NY
AREAS AFFECTED: Southern Herkimer; Southern Fulton; Montgomery; Schoharie; Western Schenectady; Western Albany; Western Greene; Western Ulster; Northern Fulton
DESCRIPTION: * WHAT...Wintry mix precipitation expected. Total snow accumulations 0.5 to 2.5 inches with locally up to 3 to 3.5 inches along the foothills of the southern Adirondacks. Ice accumulations from a glaze to around one tenth of an inch. * WHERE...The eastern Catskills, Helderbergs, Mohawk Valley and Schoharie Valley of eastern New York. * WHEN...From 9 AM Tuesday to 3 AM EST Wednesday. * IMPACTS...Plan on slippery road conditions. The hazardous conditions will likely impact today's evening commute. * ADDITIONAL DETAILS...Light snow overspread the region this morning from south to north, before mixing with sleet and freezing rain late this afternoon into this evening. Precipitation will taper off by early Wednesday morning.
INSTRUCTION: Slow down and use caution while traveling.
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Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
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
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