Weather Alert in New York
Severe Thunderstorm Warning issued April 29 at 5:12PM EDT until April 29 at 6:00PM EDT by NWS Binghamton NY
AREAS AFFECTED: Madison, NY; Oneida, NY; Onondaga, NY
DESCRIPTION: SVRBGM The National Weather Service in Binghamton has issued a * Severe Thunderstorm Warning for... Northwestern Oneida County in central New York... Northwestern Madison County in central New York... Northeastern Onondaga County in central New York... * Until 600 PM EDT. * At 512 PM EDT, severe thunderstorms were located along a line extending from near Redfield to near Central Square to near Baldwinsville to Weedsport, moving east at 40 mph. HAZARD...60 mph wind gusts and quarter size hail. SOURCE...Radar indicated. IMPACT...Hail damage to vehicles is expected. Expect wind damage to roofs, siding, and trees. * Locations impacted include... Stokes Corner, Lakeport, Westvale, Union Corners, Sylvan Beach, Bayberry, Boonville, Florence, Galeville, and Blossvale.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building.
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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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