Weather Alert in Alaska

Recent Locations: Sun Valley, ID   Council, ID   Fairbanks, AK  

Winter Weather Advisory issued August 25 at 7:58PM AKDT until August 28 at 7:00AM AKDT by NWS Fairbanks AK

AREAS AFFECTED: Central Beaufort Sea Coast; Central Arctic Plains; Central Brooks Range

DESCRIPTION: * WHAT...Mixed precipitation expected. Total snow accumulations up to 2 inch inches north of the Brooks Range and up to 1 inch in the Brooks Range and ice accumulations around a light glaze. * WHERE...Central Arctic Plains, Central Beaufort Sea Coast, and Central Brooks Range. * WHEN...From 10 PM Tuesday to 7 AM AKDT Thursday. * IMPACTS...Plan on slippery road conditions. Any accumulating snow and freezing rain could create difficult travel conditions. * ADDITIONAL DETAILS...There is very high uncertainty in exact accumulations. Freezing rain is possible everywhere, especially in the Brooks Range and along the Dalton Highway south of Prudhoe Bay. Temperatures will hover around 32 degrees, especially Tuesday night and Wednesday night which will make things difficult to accumulate unless precipitation rates are heavy enough to overcome warm ground temperatures. The greatest risk for accumulating snow will be north of the Brooks Range and towards the coast, while the greatest risk for freezing rain accumulations resides in the Brooks Range. The Dalton Highway in between has equal chances for both.

INSTRUCTION: Slow down and use caution while traveling. The latest road conditions for the state you are calling from can be obtained by calling 5 1 1.

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Weather Topic: What are Altocumulus Clouds?

Home - Education - Cloud Types - Altocumulus Clouds

Altocumulus Clouds Next Topic: Altostratus Clouds

Similar to cirrocumulus clouds, altocumulus clouds are characterized by cloud patches. They are distinguished by larger cloudlets than cirrocumulus clouds but are still smaller than stratocumulus clouds.

Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km) and may resemble, at times, the shape of a flying saucer. These uncommon formations, called altocumulus lenticularis, are created by uplift in the atmosphere and are most often seen in close proximity to mountains.

Next Topic: Altostratus Clouds

Weather Topic: What are Cirrocumulus Clouds?

Home - Education - Cloud Types - Cirrocumulus Clouds

Cirrocumulus Clouds Next Topic: Cirrostratus Clouds

Cirrocumulus clouds form at high altitudes (usually around 5 km) and have distinguishing characteristics displayed in a fine layer of small cloud patches. These small cloud patches are sometimes referred to as "cloudlets" in relation to the whole cloud formation.

Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the water droplets in the cloud freeze into ice crystals and the cloud becomes a cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud formations generally pass rapidly.

Next Topic: Cirrostratus Clouds

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