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 Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
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