Weather Alert in New York
Winter Weather Advisory issued February 5 at 12:44PM 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 Friday 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 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.
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Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
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