Weather Alert in New York
Winter Storm Warning issued February 22 at 9:49PM EST until February 24 at 6:00AM EST by NWS Buffalo NY
AREAS AFFECTED: Chautauqua
DESCRIPTION: * WHAT...Heavy snow. Total snow accumulations 8 to 12 inches in a narrow band along the Chautauqua Ridge. Snow accumulations will be much lower along the Lake Erie shore and farther inland near Jamestown, where only 2 to 4 inches is expected. * WHERE...Chautauqua County. The greatest accumulations will focus in a narrow band along the Chautauqua Ridge. * WHEN...Until 6 AM EST Tuesday. * IMPACTS...Travel will be difficult with snow covered roads and poor visibility at times. The hazardous conditions will impact the Monday morning and evening commutes.
INSTRUCTION: Widespread accumulating snow will create difficult travel conditions. Submit snow reports through our website or social media.
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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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