Weather Alert in Alaska
Winter Weather Advisory issued February 13 at 11:35AM AKST until February 14 at 6:00PM AKST by NWS Fairbanks AK
AREAS AFFECTED: Noatak Valley; Kivalina and Red Dog Dock; Lower Kobuk Valley; Baldwin Peninsula; Northern Seward Peninsula; Shishmaref; Bering Strait Coast
DESCRIPTION: * WHAT...Snow and blowing snow expected. Total snow accumulations between 2 and 5 inches. Winds gusting up to 35 mph expected, except up to 45 mph near Shungnak. * WHERE...Baldwin Peninsula, Bering Strait Coast, Kivalina and Red Dog Dock, Lower Kobuk Valley, Noatak Valley, Northern Seward Peninsula, and Shishmaref. * WHEN...From 3 PM this afternoon to 6 PM AKST Saturday. * IMPACTS...Travel may be impacted. * ADDITIONAL DETAILS...Snowfall and gusty winds could lead to visibilities reducing to 1/2 mile at times.
INSTRUCTION: Slow down and use caution while traveling. Visit 511.alaska.gov or call 5 1 1 for the latest road conditions.
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Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
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
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