Weather Alert in New York
Flood Warning issued March 9 at 4:10PM EDT until March 10 at 9:00AM EDT by NWS Burlington VT
AREAS AFFECTED: Clinton, NY
DESCRIPTION: * WHAT...Flooding caused by an ice jam is expected. * WHERE...A portion of northern New York, including the following county, Clinton. * WHEN...Until 900 AM EDT Tuesday. * IMPACTS...Flooding of rivers, creeks, streams, and other low-lying and flood-prone locations is imminent or occurring. * ADDITIONAL DETAILS... - At 408 PM EDT, Emergency management reported an ice jam near the warned area due to snowmelt. Flooding is ongoing or expected to begin shortly. - An ice jam has developed in Champlain. Based on the gage at Perry Mills, water appears to be backing up again. Emergency Management reports that the river is already near bankfull, and any discharge of water may result in flooding in the village of Champlain along the Great Chazy River. - Some locations that will experience flooding include... Champlain Village, Champlain, Mooers and Perry Mills. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles.
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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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