Weather Alert in New York
Flood Warning issued May 10 at 10:45PM EDT until May 11 at 8:00AM EDT by NWS Binghamton NY
AREAS AFFECTED: Onondaga, NY
DESCRIPTION: ...The Flood Warning continues for the following rivers in New York... Onondaga Lake At Liverpool affecting Onondaga County. Cayuga Lake At Ithaca affecting Tompkins County. * WHAT...Minor flooding is forecast. * WHERE...Onondaga Lake at Liverpool. * WHEN...Until tomorrow morning. * 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 10:30 PM EDT Saturday the stage was 366.0 feet. - Forecast...The lake is expected to rise to a crest of 366.0 feet just after midnight tonight. - Flood stage is 366.0 feet. - https://www.weather.gov/safety/flood
INSTRUCTION: Please report observed flooding to local emergency services or law enforcement and request they pass this information to the National Weather Service when you can do so safely. Additional information is available at www.weather.gov. The next statement will be issued Sunday morning at 800 AM EDT.
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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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