Weather Alert in New York
Flash Flood Warning issued March 31 at 10:42PM EDT until April 1 at 12:30AM EDT by NWS Binghamton NY
AREAS AFFECTED: Delaware, NY
DESCRIPTION: FFWBGM The National Weather Service in Binghamton has extended the * Flash Flood Warning for... Delaware County in central New York... * Until 1230 AM EDT. * At 1042 PM EDT, Doppler radar indicated another round of thunderstorms about to enter the warned area. Between 1.5 and 2 inches of rain fell earlier and an additional half inch will be possible with this next round of storms. Flash flooding is ongoing or expected to begin shortly. HAZARD...Flash flooding caused by thunderstorms. SOURCE...Radar. IMPACT...Flash flooding of small creeks and streams, urban areas, highways, streets and underpasses as well as other poor drainage and low-lying areas. * Some locations that will experience flash flooding include... Walton, Delhi, Deposit, Davenport, Roxbury, Colchester, Meredith, Andes, Stamford, Hobart, Franklin, Meridale, Downsville, Corbett, East Meredith, Bovina Center, Harvard, Sidney Center, Kortright and Hamden.
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.
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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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