Weather Alert in Alaska

Recent Locations: Surry, VA   Holtsville, NY   Arctic Village, AK  

Winter Storm Warning issued March 3 at 6:25AM AKST until March 4 at 12:00PM AKST by NWS Juneau AK

AREAS AFFECTED: Admiralty Island

DESCRIPTION: ...SNOW FOR THE NORTHERN AND CENTRAL PANHANDLE THROUGH WEDNESDAY... Another system is moving into the panhandle early this morning is bringing heavier snowfall rates across much of central and northern southeast Alaska. Snow is expected to mix with and eventually change over to rain on Tuesday from Kake over to Petersburg, however, if the changeover is delayed, snowfall amounts could be higher. * WHAT...Heavy snow expected. Total snow accumulations of 9 to 12 inches. * WHERE...Admiralty Island. * WHEN...Until noon AKST Wednesday. * IMPACTS...Travel will be very difficult and is discouraged unless it is an emergency. * ADDITIONAL DETAILS...Heaviest snowfall rates are expected Tuesday morning and afternoon, with snowfall rates of an inch an hour possible.

INSTRUCTION: If you must travel, keep an extra flashlight, food, and water with you in case of an emergency. People are urged to prepare their property before the onset of winter weather.

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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

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

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