Weather Alert in New York
Flood Watch issued February 20 at 12:47PM EST until February 21 at 8:00PM EST by NWS Binghamton NY
AREAS AFFECTED: Steuben
DESCRIPTION: An ice jam may cause water to infiltrate the lowlands along the river. * WHAT...Flooding caused by ice jams is possible. * WHERE...A portion of central New York, including the following county, Steuben. * WHEN...Through Saturday evening. * IMPACTS...The combination of recent rain and snowmelt will result in increased flow along rivers and streams in Steuben County through Saturday. Ice on the rivers may break up, jam downstream and cause flooding along the river. * ADDITIONAL DETAILS... - Ice jams have been reported by county officials along the Canisteo and Cohocton Rivers. The ice jam on the Canisteo River is located near West Cameron. The ice jam on the Cohocton River is located near the Route 4 bridge about 2 miles upstream from Coopers Plain. - 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 Precipitation?
Home - Education - Precipitation - Precipitation
Next Topic: Rain
Precipitation can refer to many different forms of water that
may fall from clouds. Precipitation occurs after a cloud has become saturated to
the point where its water particles are more dense than the air below the cloud.
In most cases, precipitation will reach the ground, but it is not uncommon for
precipitation to evaporate before it reaches the earth's surface.
When precipitation evaporates before it contacts the ground it is called Virga.
Graupel, hail, sleet, rain, drizzle, and snow are forms of precipitation, but fog
and mist are not considered precipitation because the water vapor which
constitutes them isn't dense enough to fall to the ground.
Next Topic: Rain
Weather Topic: What are Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
Next Topic: Sleet
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