Weather Alert in Alaska

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Flood Advisory issued September 4 at 12:36PM AKDT until September 6 at 12:00PM AKDT by NWS Fairbanks AK

AREAS AFFECTED: Upper Koyukuk Valley

DESCRIPTION: * WHAT...Flooding caused by excessive rainfall continues. * WHERE...Koyukuk River near Allakaket. * WHEN...Until noon AKDT Saturday. * IMPACTS...Minor flooding in low-lying and poorly drained areas. * ADDITIONAL DETAILS... - For the duration of this event there have been reports of some low lying roads being inundated. - The streamgage on the Koyukuk River below the John River shows water levels have been fluctuating less that a foot over the last 5 days and are not showing a rising or dropping trend. Though rain is still falling in areas on the south side of the Brooks Range, upstream locations (Slate Creek and the Middle and South Forks of the Koyukuk River) are not showing significant increases in response. Water levels are expected to remain steady at Allakaket for the next few days. - Http://www.weather.gov/aprfc

INSTRUCTION: N/A

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Weather Topic: What are Stratus Clouds?

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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.

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Weather Topic: What are Altocumulus Clouds?

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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.

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