Weather Alert in New York
Winter Storm Watch issued February 19 at 1:04AM EST until February 21 at 10:00AM EST by NWS Albany NY
AREAS AFFECTED: Northern Warren
DESCRIPTION: * WHAT...Heavy mixed precipitation possible. Total snow accumulations over 7 inches possible. Ice accumulations around a glaze possible. * WHERE...Northern Warren County. * WHEN...From Friday morning through Saturday morning. * IMPACTS...Travel could be difficult. The hazardous conditions could impact the Friday evening commute. * ADDITIONAL DETAILS...Precipitation will likely begin as wet snow before transitioning briefly over to a wintry mix during the afternoon hours for a mix of freezing rain/rain/snow before returning back to all snow for Friday evening. Exact amounts will greatly depend on when moisture arrives and how warm the air temperatures become.
INSTRUCTION: Monitor the latest forecasts for updates on this situation. Be prepared for slippery roads. Slow down and use caution while driving. If you are going outside, watch your first few steps taken on stairs, sidewalks, and driveways. These surfaces could be icy and slippery, increasing your risk of a fall and injury.
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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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