Weather Alert in Alaska
High Wind Warning issued February 24 at 3:58PM AKST until February 26 at 9:00AM AKST by NWS Anchorage AK
AREAS AFFECTED: Thompson Pass
DESCRIPTION: * WHAT...North winds 40 to 65 mph with gusts up to 85 mph expected. Wind chills dropping to 45 below Wednesday night. * WHERE...Thompson Pass. * WHEN...From 3 AM Wednesday to 9 AM AKST Thursday. * IMPACTS...High winds may move loose debris, damage property, and cause power outages. Travel will be difficult. Blowing snow due to high winds will reduce visibilities to one half mile or less at times. The dangerously cold wind chills as low as 40 below zero could cause frostbite on exposed skin in as little as 10 minutes. * ADDITIONAL DETAILS...North to northeast winds will rapidly strengthen late Tuesday afternoon through Tuesday night, then peak Wednesday through Wednesday night. As winds first develop, freshly fallen snow will easily blow around, leading to near-blizzard conditions at times. As snow becomes scoured out, visibilities should improve. Winds will very slowly diminish Thursday through Friday.
INSTRUCTION: Winds this strong can make driving difficult, especially for high profile vehicles. Use extra caution.
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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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