Weather Alert in Alaska
Winter Weather Advisory issued February 13 at 4:56PM AKST until February 14 at 6:00AM AKST by NWS Anchorage AK
AREAS AFFECTED: Central Alaska Peninsula; Northern Alaska Peninsula
DESCRIPTION: * WHAT...A wintry mix is expected becoming rain by Saturday morning. * WHERE...Central Alaska Peninsula and Northern Alaska Peninsula. * WHEN...Until 6 AM AKST Saturday. * IMPACTS...Snow and rain could make travel very difficult. * ADDITIONAL DETAILS...A complex weather system continues moving through the region the rest of today into Saturday. A transition to freezing rain this evening will become rain as temperatures warm above freezing by Saturday morning.
INSTRUCTION: Slow down and use caution while traveling.
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Current U.S. National Radar--Current
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National Weather Forecast--Current
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North America Water Vapor (Moisture)
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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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