Weather Alert in New York
Lake Effect Snow Warning issued March 16 at 1:54PM EDT until March 18 at 8:00AM EDT by NWS Buffalo NY
AREAS AFFECTED: Oswego
DESCRIPTION: * WHAT...Heavy lake effect snow expected. Total snow accumulations 6 to 12 inches in the most persistent bands. Winds gusting up to 45 mph will produce blowing and drifting snow late tonight through Tuesday. There may be a brief period of sleet and freezing rain during the transition to snow this evening, with ice accumulations of up to a tenth of an inch in some areas. * WHERE...Oswego County. * WHEN...From 9 PM this evening to 8 AM EDT Wednesday. * IMPACTS...Travel will be difficult with snow covered roads and poor visibility. The hazardous conditions will impact the Tuesday morning and evening commutes. Gusty winds will down tree branches and cause isolated power outages. * ADDITIONAL DETAILS...A rapid drop in temperatures late this evening may produce very icy conditions on untreated roads, sidewalks, and parking lots.
INSTRUCTION: Heavy snow will fall in relatively narrow bands. If traveling, be prepared for rapidly changing road conditions and visibilities. Submit snow reports through our website or social media.
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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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