Weather Alert in New York
Flood Warning issued April 1 at 3:32PM EDT until April 3 at 11:00AM EDT by NWS Albany NY
AREAS AFFECTED: Herkimer, NY; Oneida, NY
DESCRIPTION: * WHAT...Moderate flooding is occurring and moderate flooding is forecast. This approaches the flood of record. * WHERE...West Canada Creek at Hinckley. * WHEN...Until late Friday morning. * IMPACTS...At 1228.0 feet, Moderate flood stage. Three feet of water are spilling over and there is widespread flooding downstream between Hinckley and Herkimer. Route 28 from White Creek Road To Mechanic Street In Newport is closed due to water over the roadway. * ADDITIONAL DETAILS... - At 2:45 PM EDT Wednesday the stage was 1229.8 feet. - Forecast...The river is expected to fall below flood stage early Friday morning and continue falling to 1226.5 feet Saturday morning. - Flood stage is 1227.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: N/A
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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.
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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.
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