Weather Alert in New York
Winter Storm Watch issued February 19 at 1:04AM EST until February 21 at 10:00AM EST by NWS Albany NY
AREAS AFFECTED: Northern Warren
DESCRIPTION: * WHAT...Heavy mixed precipitation possible. Total snow accumulations over 7 inches possible. Ice accumulations around a glaze possible. * WHERE...Northern Warren County. * WHEN...From Friday morning through Saturday morning. * IMPACTS...Travel could be difficult. The hazardous conditions could impact the Friday evening commute. * ADDITIONAL DETAILS...Precipitation will likely begin as wet snow before transitioning briefly over to a wintry mix during the afternoon hours for a mix of freezing rain/rain/snow before returning back to all snow for Friday evening. Exact amounts will greatly depend on when moisture arrives and how warm the air temperatures become.
INSTRUCTION: Monitor the latest forecasts for updates on this situation. 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 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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