Weather Alert in New York
Winter Weather Advisory issued February 6 at 1:59AM EST until February 7 at 7:00PM EST by NWS Buffalo NY
AREAS AFFECTED: Niagara; Orleans; Northern Erie; Genesee; Wyoming; Chautauqua; Cattaraugus; Southern Erie
DESCRIPTION: * WHAT...A combination of widespread snow and localized lake effect snow expected. Total snow accumulations 3 to 6 inches expected, with locally higher amounts possible across the hilltops south of Buffalo. Winds gusting as high as 40 mph will create areas of blowing and drifting snow. * WHERE...Erie, Niagara, Orleans, Genesee, Wyoming, Chautauqua, and Cattaraugus Counties. * WHEN...From 7 AM this morning to 7 PM EST Saturday. * IMPACTS...Travel will be difficult. The hazardous conditions will impact the Friday evening commute. * ADDITIONAL DETAILS...An Arctic front will bring widespread snow showers to the region this morning, which will then taper off to more localized lake effect snow tonight through Saturday. Winds strengthening behind this front late this 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.
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North America Water Vapor (Moisture)
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Weather Topic: What is Evaporation?
Home - Education - Precipitation - Evaporation
Next Topic: Fog
Evaporation is the process which returns water from the earth
back to the atmosphere, and is another crucial process in the water cycle.
Evaporation is the transformation of liquid into gas, and it happens because
molecules are excited by the application of energy and turn into vapor.
In order for water to evaporate it has to be on the surface of a body of water.
Next Topic: Fog
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
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