Weather Alert in New York
Winter Storm Warning issued February 20 at 4:01AM EST until February 21 at 1:00PM EST by NWS Albany NY
AREAS AFFECTED: Hamilton; Northern Warren; Southeast Warren; Bennington; Western Windham; Eastern Windham
DESCRIPTION: * WHAT...Heavy mixed precipitation expected. Total snow accumulations between 7 and 10 inches. For Bennington county in southern Vermont, snow accumulations between 6 and 10 inches for elevations above 1500 feet. Ice accumulations around one tenth of an inch. * WHERE...In New York, Warren and Hamilton counties. In Vermont, Windham County and elevations above 1500 feet in Bennington County. * WHEN...From 10 AM this morning to 1 PM EST Saturday. * IMPACTS...Roads, and especially bridges and overpasses, will likely become slick and hazardous. Travel could be difficult. The hazardous conditions could impact this evening's commute. * ADDITIONAL DETAILS...Snowfall rates could range between 0.5 inches to 1 inch per hour this evening into tonight across the highest elevations of Bennington county and across Windham county in southern Vermont and across northern Warren county.
INSTRUCTION: If you must travel, keep an extra flashlight, food, and water in your vehicle in case of an emergency.
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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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