Weather Alert in New York
Wind Advisory issued March 15 at 11:12AM EDT until March 17 at 11:00AM EDT by NWS Burlington VT
AREAS AFFECTED: Northern St. Lawrence; Eastern Clinton; Southeastern St. Lawrence; Eastern Essex; Southwestern St. Lawrence; Grand Isle; Western Franklin; Western Chittenden; Eastern Franklin; Eastern Chittenden; Eastern Addison
DESCRIPTION: * WHAT...South winds 20 to 30 mph with gusts 45 to 55 mph expected. * WHERE...Portions of northern New York and central and northwest Vermont. * WHEN...From 11 PM this evening to 11 AM EDT Tuesday. * IMPACTS...Gusty winds will blow around unsecured objects. Tree limbs could be blown down and a few power outages may result. * ADDITIONAL DETAILS...Two period of strong winds are expected, the first will be between midnight tonight and 10 AM Monday, followed by another period of strong winds between 8 PM Monday evening and 8 AM Tuesday.
INSTRUCTION: Winds this strong can make driving difficult, especially for high profile vehicles. Use extra caution. Secure outdoor objects.
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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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