Weather Alert in New York
Flood Watch issued February 21 at 10:55AM EST until February 21 at 8:00PM EST by NWS Binghamton NY
AREAS AFFECTED: Steuben; Tompkins
DESCRIPTION: An ice jam may cause water to infiltrate the lowlands along the river. * WHAT...Flooding caused by ice jams continues to be possible. * WHERE...A portion of central New York, including the following counties, Steuben and Tompkins. * WHEN...Until 8 PM EST this evening. * IMPACTS...The combination of recent rain and snowmelt has resulted in increased flow along rivers and streams in Tompkins and Steuben counties. Ice on the rivers may break up, and jam downstream to cause flooding in some low lying areas along the river. Some park and trail areas have already experienced elevated water levels. * ADDITIONAL DETAILS... - For Steuben County, ice jams have been reported by county officials along the Canisteo and Cohocton Rivers, including near Cameron Mills, Campbell, West Cameron, and Coopers Plains. For Tompkins County, an ice jam have been reported by county officials along Fall Creek near Beebe Lake and Cornell University in Ithaca. - https://www.weather.gov/safety/flood
INSTRUCTION: You should monitor later forecasts and be alert for possible Flood Warnings. Those living in areas prone to flooding should be prepared to take action should flooding develop.
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Weather Topic: What is Condensation?
Home - Education - Precipitation - 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
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.
Next Topic: Cumulus Clouds
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