Weather Alert in Alaska
Blizzard Warning issued February 5 at 2:18PM AKST until February 6 at 3:00PM AKST by NWS Fairbanks AK
AREAS AFFECTED: Western Arctic Coast
DESCRIPTION: * WHAT...Blowing snow leading to blizzard conditions, especially near Point Lay. East-northeast winds gusting as high as 55 mph. * WHERE...Point Lay and Point Hope. * WHEN...Until 3 PM AKST Friday. * IMPACTS...Travel could be very difficult. Areas of blowing snow could significantly reduce visibility. * ADDITIONAL DETAILS...A shallow ground blizzard is expected to continue at Point Lay through at least Friday morning. Winds will slowly weaken through the day Friday allowing conditions to slowly improve. There is a chance for periods of blowing snow to impact Point Hope as well, although these will be less frequent and less impactful.
INSTRUCTION: If you must travel, keep an extra flashlight, food, and water in your vehicle in case of an emergency.
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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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