Weather Alert in New York
Flood Warning issued May 9 at 11:20AM EDT until May 11 at 11:00AM EDT by NWS Binghamton NY
AREAS AFFECTED: Broome, NY; Tioga, NY
DESCRIPTION: ...The National Weather Service in Binghamton NY has issued a Flood Warning for the following rivers in New York...Pennsylvania... Susquehanna River At Conklin affecting Broome and Susquehanna Counties. Susquehanna River At Vestal affecting Broome and Tioga Counties. * WHAT...Minor flooding is forecast. * WHERE...Susquehanna River at Vestal. * WHEN...From Saturday morning to late Sunday morning. * IMPACTS...At 18.0 feet, Flood stage. The river overflows banks and lowland flooding begins within the flood plain. * ADDITIONAL DETAILS... - At 10:00 AM EDT Friday the stage was 14.2 feet. - Forecast...The river is expected to rise above flood stage tomorrow morning to a crest of 18.4 feet early tomorrow afternoon. It will then fall below flood stage late tomorrow evening. - Flood stage is 18.0 feet. - https://www.weather.gov/safety/flood
INSTRUCTION: Motorists should not attempt to drive around barricades or drive cars through flooded areas. Caution is urged when walking near riverbanks. Additional information is available at www.weather.gov. The next statement will be issued this evening at 1100 PM EDT.
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Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
Weather Topic: What is Graupel?
Home - Education - Precipitation - Graupel
Next Topic: Hail
Graupel is a form of precipitation that is created by atmospheric conditions
which cause supercooled water droplets to contact snow crystals and freeze to
their surface.
Sometimes known as soft hail or snow pellets, graupel is delicate and easily
destroyed by touch. Whereas hail usually falls during severe weather, graupel
doesn't require such conditions to form, and can form in mild precipitation
similar to situations which produce snowfall.
Next Topic: Hail
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