Weather Alert in New York
Flood Warning issued June 22 at 9:09PM EDT until June 23 at 8:00AM EDT by NWS Binghamton NY
AREAS AFFECTED: Chenango, NY
DESCRIPTION: ...The Flood Warning continues for the following rivers in New York... Chenango River At Sherburne affecting Chenango County. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Chenango River at Sherburne. * WHEN...Until tomorrow morning. * IMPACTS...At 9.5 feet, Water covers Blanding Road near State Highway 12, South Cross Road, Conley Road, and the north end of Williams Road. Water begins seeping across north Main Street from downtown Sherburne to the Big M. * ADDITIONAL DETAILS... - At 8:46 PM EDT Sunday the stage was 9.5 feet. - Forecast...The river is expected to fall below flood stage tomorrow morning and continue falling to 6.6 feet Wednesday 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. Additional information is available at www.weather.gov. The next statement will be issued Monday morning at 800 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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