Weather Alert in New York
Flood Watch issued March 11 at 9:09PM EDT until March 12 at 5:00PM EDT by NWS Binghamton NY
AREAS AFFECTED: Northern Oneida; Southern Oneida
DESCRIPTION: Heavy rain may fall on a deep primed snowpack leading to the melt increasing. Flows in rivers may increase quickly and reach critical levels. * WHAT...Flooding caused by rain and snowmelt continues to be possible. * WHERE...A portion of central New York, including the following areas, Northern Oneida and Southern Oneida. * WHEN...Through Thursday afternoon. * IMPACTS...Excessive runoff from heavy rain and snowmelt may result in flooding of rivers, creeks, streams, and other low-lying and flood-prone locations. Ice jams will also be possible in areas where significant ice remains. * ADDITIONAL DETAILS... - Between three quarters of an inch and one inch of rain is expected through Thursday morning. This rain combined with warm temperatures will result in significant snowmelt. This will cause rises on the Black River, Mohawk River, as well as other smaller tributaries. - https://www.weather.gov/safety/flood
INSTRUCTION: You should monitor later forecasts and be alert for possible Flood Warnings. Those living in areas prone to flooding should be prepared to take action should flooding develop.
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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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