Weather Alert in New York
Flood Warning issued March 31 at 11:05PM EDT until April 1 at 5:27PM EDT by NWS Buffalo NY
AREAS AFFECTED: Erie, NY; Wyoming, NY
DESCRIPTION: ...Forecast flooding changed from Minor to Moderate severity and increased in duration for the following rivers in New York... Cayuga Creek Near Lancaster affecting Erie and Wyoming Counties. For the Cayuga Creek...including Lancaster...Moderate flooding is forecast. * WHAT...Minor flooding is occurring and moderate flooding is forecast. * WHERE...Cayuga Creek near Lancaster. * WHEN...From this evening to Wednesday afternoon. * IMPACTS...At 10.0 feet, Moderate flood, flooding of backyards, basements and streets in Village of Lancaster. Some flooding of low lying areas in Alden, Marilla, and Cheektowaga, especially near Bowen Road and Transit Road. Some flooding possible near Union Road too. * ADDITIONAL DETAILS... - At 10:30 PM EDT Tuesday the stage was 8.84 feet. - Bankfull stage is 8.0 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 10:30 PM EDT Tuesday was 8.84 feet. - Forecast...The river is expected to rise to a crest of 10.2 feet just after midnight tonight. It will then fall below flood stage late tomorrow morning. - Flood stage is 8.0 feet. - Flood History...This crest compares to a previous crest of 10.1 feet on 06/23/1972. - 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 Wednesday morning by 1115 AM EDT.
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Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
Weather Topic: What are Altostratus Clouds?
Home - Education - Cloud Types - Altostratus Clouds
Next Topic: Cirrocumulus Clouds
Altostratus clouds form at mid to high-level altitudes
(between 2 and 7 km) and are created by a warm, stable air mass which causes
water vapor
to condense as it rise through the atmosphere. Usually altostratus clouds are
featureless sheets characterized by a uniform color.
In some cases, wind punching through the cloud formation may give it a waved
appearance, called altostratus undulatus. Altostratus clouds
are commonly seen with other cloud formations accompanying them.
Next Topic: Cirrocumulus Clouds
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