Weather Alert in New York
Winter Storm Warning issued February 20 at 1:24PM 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...Snow along with patchy sleet and freezing rain. Additional snow and sleet accumulations between 4 and 8 inches and flat ice accumulations from a glaze up to one tenth of an inch. Highest amounts in Bennington County will be mainly for elevations above 1500ft. * WHERE...Hamilton and Warren County in eastern NY and southern Vermont. * WHEN...Until 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 today's evening commute. * ADDITIONAL DETAILS...Snowfall rates could range between 0.5 inches to 1 inch per hour into tonight.
INSTRUCTION: If you must travel, keep an extra flashlight, food, and water in your vehicle in case of an emergency. Be prepared for slippery roads. Slow down and use caution while driving. If you are going outside, watch your first few steps taken on stairs, sidewalks, and driveways. These surfaces could be icy and slippery, increasing your risk of a fall and injury.
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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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