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 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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