Weather Alert in New York
Flood Warning issued April 1 at 12:26AM EDT until April 1 at 9:15AM EDT by NWS Binghamton NY
AREAS AFFECTED: Cayuga, NY
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall has caused the Owasco Inlet at Moravia to surpass major flood stage of 9.5 feet and the gauge is currently reading water levels around 10.5 feet. * WHERE...The Owasco Inlet at Moravia in Cayuga County. * WHEN...Until 915 AM EDT Wednesday. * IMPACTS...Several roads are currently flooded and closed in the vicinity of the Owasco Inlet at Moravia. * ADDITIONAL DETAILS... - At 1216 AM EDT, Over 3 inches of rain fell across the area today and flooding is ongoing in the warned area. - Rainfall has ended and flood waters will continue to recede through the overnight hours. - Some locations that will experience flooding include... Locke, Moravia, Cascade and Fillmore Glen State Park. - https://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles.
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Weather Topic: What is Evaporation?
Home - Education - Precipitation - Evaporation
Next Topic: Fog
Evaporation is the process which returns water from the earth
back to the atmosphere, and is another crucial process in the water cycle.
Evaporation is the transformation of liquid into gas, and it happens because
molecules are excited by the application of energy and turn into vapor.
In order for water to evaporate it has to be on the surface of a body of water.
Next Topic: Fog
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
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