Weather Alert in New York
Flood Warning issued April 1 at 5:28AM EDT until April 1 at 10:47AM EDT by NWS Buffalo NY
AREAS AFFECTED: Erie, NY; Wyoming, NY
DESCRIPTION: ...The Flood Warning continues for the following rivers in New York... Cayuga Creek Near Lancaster affecting Erie and Wyoming Counties. * WHAT...Minor flooding is occurring. * WHERE...Cayuga Creek near Lancaster. * WHEN...Until late this morning. * IMPACTS...At 8.0 feet, Flood stage, minor flooding in low lying areas of Lancaster and Alden. * ADDITIONAL DETAILS... - At 4:30 AM EDT Wednesday the stage was 8.1 feet and falling. - Bankfull stage is 8.0 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 4:30 AM EDT Wednesday was 9.73 feet. - Forecast...The river is expected to fall below flood stage early this morning, and continue to fall below 6 feet by this evening. - Flood stage is 8.0 feet. - Flood History...This crest compares to a previous crest of 8.1 feet on 03/15/2007. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Be especially cautious at night when it is harder to recognize the dangers of flooding. Caution is urged when walking near riverbanks. Additional information is available at www.weather.gov. The next statement will be issued this morning by 1100 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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