Weather Alert in New York
Winter Weather Advisory issued February 10 at 12:39PM EST until February 11 at 7:00AM EST by NWS Burlington VT
AREAS AFFECTED: Northern St. Lawrence; Northern Franklin; Southeastern St. Lawrence; Southern Franklin; Western Clinton; Western Essex; Southwestern St. Lawrence
DESCRIPTION: * WHAT...Snow expected. Total snow accumulations between 3 and 6 inches, with locally higher amounts in the northern Adirondacks. * WHERE...The St. Lawrence Valley and northern Adirondacks. * WHEN...Until 7 AM EST Wednesday. * IMPACTS...The heaviest snowfall rates are expected to occur this afternoon and during the evening commute. Slow travel conditions can be expected. Roads will likely become slick and hazardous. * ADDITIONAL DETAILS...Snowfall rates of 1 inch per hour are expected late this afternoon into early this evening.
INSTRUCTION: Slow down and use caution while traveling. For the latest on road conditions in New York, visit https://511ny.org.
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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
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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