Weather Alert in New York
Flood Watch issued July 13 at 1:23AM EDT until July 14 at 5:00AM EDT by NWS Binghamton NY
AREAS AFFECTED: Northern Oneida; Yates; Seneca; Southern Cayuga; Onondaga; Steuben; Schuyler; Tompkins; Madison; Southern Oneida
DESCRIPTION: * WHAT...Flash flooding caused by excessive rainfall is possible. * WHERE...A portion of central New York, including the following areas, Madison, Northern Oneida, Onondaga, Schuyler, Seneca, Southern Cayuga, Southern Oneida, Steuben, Tompkins and Yates. * WHEN...From 11 AM EDT this morning through late tonight. * IMPACTS...Excessive runoff may result in flooding of rivers, creeks, streams, and other low-lying and flood-prone locations. Flooding may occur in poor drainage and urban areas. * ADDITIONAL DETAILS... - Showers and thunderstorms developing across the area can be slow-moving and lead to heavy rainfall and instances of flash flooding. Rainfall rates can near, or exceed 1 inch per hour at times. Multiple rounds of thunderstorms training over the same area can also result in localized flooding. - https://www.weather.gov/safety/flood
INSTRUCTION: You should monitor later forecasts and be prepared to take action should Flash Flood Warnings be issued.
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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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