Weather Alert in New York
Winter Weather Advisory issued April 3 at 2:28AM EDT until April 3 at 11:00AM EDT by NWS Burlington VT
AREAS AFFECTED: Southeastern St. Lawrence; Southern Franklin; Western Clinton; Western Essex; Orleans; Essex; Lamoille; Caledonia; Washington; Orange; Eastern Addison; Eastern Rutland; Western Windsor; Eastern Windsor
DESCRIPTION: * WHAT...Mixed precipitation. Additional snow accumulations up to one inch and ice accumulations of a light glaze to around two tenths of an inch. Winds gusting as high as 35 mph. * WHERE...Portions of northern New York and along and east of the Green Mountains in Vermont, including the Northeast Kingdom. * WHEN...Until 11 AM EDT this morning. * IMPACTS...Localized areas of slick travel possible, especially bridges and overpasses. A few power outages possible due to ice accumulation and wind gusts. * ADDITIONAL DETAILS...A wintry mix of snow, sleet, and freezing rain will transition to all rain over northern New York by 7 AM and across Vermont by 9 AM this morning.
INSTRUCTION: Slow down and use caution while traveling. 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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