Weather Alert in New York
Flood Warning issued May 10 at 7:01AM EDT until May 11 at 8:00PM EDT by NWS Binghamton NY
AREAS AFFECTED: Onondaga, NY
DESCRIPTION: ...The Flood Warning continues for the following rivers in New York... East Branch Delaware At Harvard affecting Delaware County. Onondaga Lake At Liverpool affecting Onondaga County. Cayuga Lake At Ithaca affecting Tompkins County. Additional information is available at www.weather.gov. The next statement will be issued this evening at 715 PM EDT. * WHAT...Minor flooding is forecast. * WHERE...Onondaga Lake at Liverpool. * WHEN...Until 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 6:30 AM EDT Saturday the stage was 365.4 feet. - Forecast...The lake 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 Cirrus Clouds?
Home - Education - Cloud Types - Cirrus Clouds
Next Topic: Condensation
Cirrus clouds are high-level clouds that occur above 20,000 feet
and are composed mainly of ice crystals.
They are thin and wispy in appearance.
What do they indicate?
They are often the first sign of an approaching storm.
Next Topic: Condensation
Weather Topic: What are Contrails?
Home - Education - Cloud Types - Contrails
Next Topic: Cumulonimbus Clouds
A contrail is an artificial cloud, created by the passing of an
aircraft.
Contrails form because water vapor in the exhaust of aircraft engines is suspended
in the air under certain temperatures and humidity conditions. These contrails
are called exhaust contrails.
Another type of contrail can form due to a temporary reduction in air pressure
moving over the plane's surface, causing condensation.
These are called aerodynamic contrails.
When you can see your breath on a cold day, it is also because of condensation.
The reason contrails last longer than the condensation from your breath is
because the water in contrails freezes into ice particles.
Next Topic: Cumulonimbus Clouds
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