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 Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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