Weather Alert in Alaska

Recent Locations: Greenfield, IN   Winneconne, WI   Eagle River, AK  

Hydrologic Outlook issued August 30 at 11:56AM AKDT by NWS Fairbanks AK

AREAS AFFECTED: South Slopes Of The Central Brooks Range; South Slopes of the Western Brooks Range; Noatak Valley; Lower Kobuk Valley; Upper Kobuk Valleys; Lower Koyukuk Valley; Upper Koyukuk Valley

DESCRIPTION: ESFAFG The headwater tributaries of the Koyukuk, Kobuk, and Noatak Rivers have received substantial rainfall this week leading to record crests at Slate Creek near Coldfoot (30 years of record) and Dahl Creek near Kobuk (39 years of record). The crests from the early week rainfall are making their way down the main stems of the Kobuk, Koyukuk, and Noatak Rivers. Rain is expected to return Saturday afternoon with 1 to 2 inches of additional rainfall expected through Tuesday. River levels are now expected to remain high through the middle of next week.

INSTRUCTION: N/A

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Weather Topic: What is Precipitation?

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Precipitation Next Topic: Rain

Precipitation can refer to many different forms of water that may fall from clouds. Precipitation occurs after a cloud has become saturated to the point where its water particles are more dense than the air below the cloud.

In most cases, precipitation will reach the ground, but it is not uncommon for precipitation to evaporate before it reaches the earth's surface. When precipitation evaporates before it contacts the ground it is called Virga. Graupel, hail, sleet, rain, drizzle, and snow are forms of precipitation, but fog and mist are not considered precipitation because the water vapor which constitutes them isn't dense enough to fall to the ground.

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Weather Topic: What are Shelf Clouds?

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Shelf Clouds Next Topic: Sleet

A shelf cloud is similar to a wall cloud, but forms at the front of a storm cloud, instead of at the rear, where wall clouds form.

A shelf cloud is caused by a series of events set into motion by the advancing storm; first, cool air settles along the ground where precipitation has just fallen. As the cool air is brought in, the warmer air is displaced, and rises above it, because it is less dense. When the warmer air reaches the bottom of the storm cloud, it begins to cool again, and the resulting condensation is a visible shelf cloud.

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