Weather Alert in New York
Lake Effect Snow Warning issued March 16 at 1:54PM EDT until March 17 at 8:00PM EDT by NWS Buffalo NY
AREAS AFFECTED: Jefferson; Lewis
DESCRIPTION: * WHAT...Heavy lake effect snow expected. Total snow accumulations 6 to 12 inches in the most persistent bands across the Tug Hill Plateau, with 3 to 5 inches elsewhere. Winds gusting as high as 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...Jefferson and Lewis Counties. * WHEN...From 9 PM this evening to 8 PM EDT Tuesday. * 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 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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