Weather Alert in New York
Winter Storm Warning issued February 20 at 1:30AM EST until February 21 at 10:00AM EST by NWS Burlington VT
AREAS AFFECTED: Northern St. Lawrence; Eastern Clinton; Southern Franklin; Western Clinton; Orange
DESCRIPTION: * WHAT...Heavy snow expected. Total snow accumulations between 5 and 9 inches. * WHERE...In New York, Eastern Clinton, Northern St. Lawrence, Southern Franklin, and Western Clinton Counties. In Vermont, Orange County. * WHEN...From 10 AM this morning to 10 AM EST Saturday. * IMPACTS...Travel could be very difficult. The hazardous conditions will impact the evening commute. * ADDITIONAL DETAILS...Snow will be initially wet, and snowfall rates will likely exceed 1 inch per hour this evening. Snow will trend lighter and become increasingly dry tonight into Saturday. Isolated power outages could occur due to the weight of the snow.
INSTRUCTION: If you must travel, keep an extra flashlight, food, and water in your vehicle in case of an emergency. For the latest on road conditions in Vermont, visit https://newengland511.org and for New York, visit https://511ny.org.
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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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