Weather Alert in New York
Flood Warning issued April 1 at 12:26AM EDT until April 1 at 9:15AM EDT by NWS Binghamton NY
AREAS AFFECTED: Cayuga, NY
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall has caused the Owasco Inlet at Moravia to surpass major flood stage of 9.5 feet and the gauge is currently reading water levels around 10.5 feet. * WHERE...The Owasco Inlet at Moravia in Cayuga County. * WHEN...Until 915 AM EDT Wednesday. * IMPACTS...Several roads are currently flooded and closed in the vicinity of the Owasco Inlet at Moravia. * ADDITIONAL DETAILS... - At 1216 AM EDT, Over 3 inches of rain fell across the area today and flooding is ongoing in the warned area. - Rainfall has ended and flood waters will continue to recede through the overnight hours. - Some locations that will experience flooding include... Locke, Moravia, Cascade and Fillmore Glen State Park. - https://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 Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
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
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