Weather Alert in New York
Flood Warning issued May 10 at 3:16AM EDT until May 11 at 8:00PM EDT by NWS Binghamton NY
AREAS AFFECTED: Onondaga, NY
DESCRIPTION: ...The National Weather Service in Binghamton NY has issued a Flood Warning for the following rivers in New York... Onondaga Lake At Liverpool affecting Onondaga County. Additional information is available at www.weather.gov. The next statement will be issued this afternoon at 330 PM EDT. * WHAT...Minor flooding is forecast. * WHERE...Onondaga Lake at Liverpool. * WHEN...From this morning to tomorrow evening. * IMPACTS...At 366.0 feet, Minor flood stage. Trails at Onondaga Lake Park are flooded. Marina usage is also impacted. Areas downstream of the lake, in the vicinity of Hayes Road, may be affected by flood waters. * ADDITIONAL DETAILS... - At 2:30 AM EDT Saturday the stage was 365.4 feet. - Forecast...The river is expected to rise above flood stage this morning to a crest of 366.1 feet this evening. It will then fall below flood stage early tomorrow afternoon. - Flood stage is 366.0 feet. - https://www.weather.gov/safety/flood
INSTRUCTION: N/A
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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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