Weather Alert in New York

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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 Condensation?

Home - Education - Precipitation - Condensation

Condensation Next Topic: Contrails

Condensation is the process which creates clouds, and therefore it is a crucial process in the water cycle. Condensation is the change of matter from a state of gas into a state of liquid, and it happens because water molecules release heat into the atmosphere and become organized into a more closely packed structure, what we might see as water droplets.

Water is always present in the air around us as a vapor, but it's too small for us to see. When water undergoes the process of condensation it becomes organized into visible water droplets. You've probably seen condensation happen before on the surface of a cold drink!

Next Topic: Contrails

Weather Topic: What are Cumulonimbus Clouds?

Home - Education - Cloud Types - Cumulonimbus Clouds

Cumulonimbus Clouds Next Topic: Cumulus Clouds

The final form taken by a growing cumulus cloud is the cumulonimbus cloud, which is very tall and dense. The tower of a cumulonimbus cloud can soar 23 km into the atmosphere, although most commonly they stop growing at an altitude of 6 km.

Even small cumulonimbus clouds appear very large in comparison to other cloud types. They can signal the approach of stormy weather, such as thunderstorms or blizzards.

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