Weather Alert in New York
Flood Warning issued March 31 at 9:52PM EDT until April 2 at 8:00AM EDT by NWS Binghamton NY
AREAS AFFECTED: Chenango, NY
DESCRIPTION: ...The Flood Warning is extended for the following rivers in New York... Chenango River At Sherburne affecting Chenango County. * WHAT...Minor flooding is forecast. * WHERE...Chenango River at Sherburne. * WHEN...From late tonight to Thursday morning. * IMPACTS...At 8.5 feet, Water spreads throughout agricultural lands nearest the river on the West side of Sherburne. * ADDITIONAL DETAILS... - At 9:30 PM EDT Tuesday the stage was 7.5 feet. - Forecast...The river is expected to rise above flood stage just after midnight tonight to a crest of 9.0 feet tomorrow morning. It will then fall below flood stage tomorrow evening. - Flood stage is 8.5 feet. - https://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Please report observed flooding to local emergency services or law enforcement and request they pass this information to the National Weather Service when you can do so safely. Additional information is available at www.weather.gov. The next statement will be issued Wednesday morning at 1000 AM EDT.
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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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