Weather Alert in New York
Flood Watch issued February 21 at 2:42AM 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 an ice jam continues to be possible. * WHERE...A portion of central New York, including the following counties, Steuben and Tompkins. * WHEN...Through this evening. * IMPACTS...The combination of recent rain and snowmelt will result in increased flow along rivers and streams in Tompkins and Steuben counties through Saturday. Ice on the rivers may break up, jam downstream and cause flooding along the river. * ADDITIONAL DETAILS... - For Steuben County, ice jams have been reported by county officials along the Canisteo and Cohocton Rivers. The ice jam on the CanisteoRiver is located near West Cameron. The ice jam on theCohocton River is located near the Route 4 bridge about 2 miles upstream from Coopers Plain. For Tompkins County, ice jams have been reported by county officials along the Fall Creek in Ithaca. The ice jam on Fall Creek is located 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 are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
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