Weather Alert in New York
Winter Storm Warning issued February 22 at 1:03AM EST until February 23 at 7:00PM EST by NWS Albany NY
AREAS AFFECTED: Schoharie; Western Schenectady; Western Albany; Eastern Rensselaer; Bennington; Western Windham; Eastern Windham
DESCRIPTION: * WHAT...Heavy snow expected. Total snow accumulations between 5 and 12 inches with locally higher amounts into the Helderbergs and Schoharie County. Winds gusting between 30 and 40 mph will lead to areas of blowing snow. * WHERE...Schoharie, Western Schenectady, Western Albany and Eastern Rensselaer Counties in eastern New York and all of southern Vermont. * WHEN...From 7 PM this evening to 7 PM EST Monday. * IMPACTS...Travel could be difficult. The hazardous conditions could impact the Monday morning and evening commutes. * ADDITIONAL DETAILS...A powerful nor'easter will impact the region late this afternoon through Monday. The higher snowfall amounts will be favored across the higher elevations. Snowfall rates may reach 1 inch per hour at times tonight into early Monday morning with up to 2 inches in the Helderbergs and Schoharie 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 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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