Weather Alert in New York
Flood Warning issued May 9 at 10:42PM EDT until May 11 at 8:00AM EDT by NWS Binghamton NY
AREAS AFFECTED: Delaware, NY
DESCRIPTION: ...The Flood Warning continues for the following rivers in New York... East Branch Delaware At Harvard affecting Delaware County. Cayuga Lake At Ithaca affecting Tompkins County. ...The Flood Warning is cancelled for the following rivers in Pennsylvania...New York... Susquehanna River At Conklin affecting Broome and Susquehanna Counties. Susquehanna River At Vestal affecting Broome and Tioga Counties. * WHAT...Minor flooding is forecast. * WHERE...East Branch Delaware at Harvard. * WHEN...From Saturday afternoon to Sunday morning. * IMPACTS...At 10.0 feet, Minor flood stage. Low lying roads along the river from Downsville to East Branch begin to flood. * ADDITIONAL DETAILS... - At 9:45 PM EDT Friday the stage was 7.6 feet. - Forecast...The river is expected to rise to a crest of 10.0 feet early tomorrow afternoon. It will then fall below flood stage tomorrow evening. - Flood stage is 10.0 feet. - https://www.weather.gov/safety/flood
INSTRUCTION: Caution is urged when walking near riverbanks. 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. Motorists should not attempt to drive around barricades or drive cars through flooded areas. Additional information is available at www.weather.gov. The next statement will be issued this evening at 1145 PM EDT.
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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
Weather Topic: What are Cumulus Clouds?
Home - Education - Cloud Types - Cumulus Clouds
Next Topic: Drizzle
Cumulus clouds are fluffy and textured with rounded tops, and
may have flat bottoms. The border of a cumulus cloud
is clearly defined, and can have the appearance of cotton or cauliflower.
Cumulus clouds form at low altitudes (rarely above 2 km) but can grow very tall,
becoming cumulus congestus and possibly the even taller cumulonimbus clouds.
When cumulus clouds become taller, they have a greater chance of producing precipitation.
Next Topic: Drizzle
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