Weather Alert in Alaska
Winter Weather Advisory issued March 29 at 11:35AM AKDT until March 30 at 5:00PM AKDT by NWS Anchorage AK
AREAS AFFECTED: Kodiak Island Southwest
DESCRIPTION: * WHAT...Snow expected. Total snow accumulation 4 to 10 inches. Highest accumulations along the Gulf side of the island. * WHERE...Kodiak Island Southwest. * WHEN...Until 5 PM AKDT Monday. * IMPACTS...Travel could be very difficult. * ADDITIONAL DETAILS...Heaviest snowfall rates expected this afternoon and evening. Less snowfall, 1 to 2 inches, is expected for areas on the Shelikof Strait side of the island, such as Karluk and Larsen Bay. Moderate snow rates will be maintained in and around Old Harbor through Monday morning. Steady snow will become more showery and lighter by late Monday afternoon and tapers off fully through Monday night.
INSTRUCTION: Slow down and use caution while traveling. For the latest road conditions call 5 1 1 or visit 511.alaska.gov.
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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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