Weather Alert in New York
Special Weather Statement issued September 4 at 2:36PM EDT by NWS Burlington VT
AREAS AFFECTED: Northern St. Lawrence; Southeastern St. Lawrence; Southwestern St. Lawrence
DESCRIPTION: At 236 PM EDT, Doppler radar was tracking strong thunderstorms along a line extending from 6 miles north of Morristown Village to 9 miles northeast of Fort Drum to 6 miles northeast of Barnes Corners. Movement was northeast at 60 mph. HAZARD...Wind gusts up to 50 mph. SOURCE...Radar indicated. IMPACT...Gusty winds could knock down tree limbs and blow around unsecured objects. Locations impacted include... Morristown Village, Richville, Canton Village, Gouverneur Village, Rensselaer Falls, Norwood, Hammond Village, Potsdam Village, Heuvelton, Hermon Village, De Peyster, Potsdam, Pierrepont, Waddington, Russell, Madrid, Clare, Gouverneur, Hermon, and Macomb.
INSTRUCTION: If outdoors, consider seeking shelter inside 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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