Weather Alert in Alaska

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Winter Weather Advisory issued February 23 at 3:39PM AKST until February 24 at 4:00PM AKST by NWS Anchorage AK

AREAS AFFECTED: Central Copper Valley; Tok Cutoff

DESCRIPTION: * WHAT...Snow expected. Total snow accumulations between 2 and 6 inches from Glennallen to Gakona and 6 to 12 inches along the Tok Cutoff. * WHERE...Central Copper Valley and Tok Cutoff, including Glennallen, Gakona, Chistochina, and Slana. * WHEN...Until 4 PM AKST Tuesday. * IMPACTS...Travel could be very difficult. Visibility reduced to one half mile or less at times. * ADDITIONAL DETAILS...The heaviest snow will be this evening through the overnight hours. The area of highest accumulation is expected along the Tok Cutoff from around Chistochina to Slana. Much less snow is expected as you head south from Glennallen down to Chitina. Snow will gradually taper off during the day Tuesday. However, gusty northwest to northeast winds will develop and lead to reduced visibilities as the freshly fallen snow is lofted and blown around. The gusty winds and blowing snow will likely continue through Tuesday night and perhaps beyond.

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 is Snow?

Home - Education - Precipitation - Snow

Snow Next Topic: Stratocumulus Clouds

Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake, has unique characteristics, but all of them grow in a hexagonal structure. Snowfall can last for sustained periods of time and result in significant buildup of snow on the ground.

On the earth's surface, snow starts out light and powdery, but as it begins to melt it tends to become more granular, producing small bits of ice which have the consistency of sand. After several cycles of melting and freezing, snow can become very dense and ice-like, commonly known as snow pack.

Next Topic: Stratocumulus Clouds

Weather Topic: What are Stratus Clouds?

Home - Education - Cloud Types - Stratus Clouds

Stratus Clouds Next Topic: Wall Clouds

Stratus clouds are similar to altostratus clouds, but form at a lower altitude and are identified by their fog-like appearance, lacking the distinguishing features of most clouds.

Stratus clouds are wider than most clouds, and their base has a smooth, uniform look which is lighter in color than a nimbostratus cloud. The presence of a stratus cloud indicates the possibility of minor precipitation, such as drizzle, but heavier precipitation does not typically arrive in the form of a stratus cloud.

Next Topic: Wall Clouds

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