Weather Alert in Alaska

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Coastal Flood Advisory issued August 24 at 11:09PM AKDT until August 25 at 6:00PM AKDT by NWS Anchorage AK

AREAS AFFECTED: Kuskokwim Delta Coast and Nunivak Island

DESCRIPTION: * WHAT...Water levels 1.5 to 2.5 feet above the normal highest tide line. * WHERE...Along the Kuskokwim Delta coast, including the communities of Kipnuk, Kwigillingok, and Kongiganak. * WHEN...11 AM AKDT Monday through 6 PM AKDT Monday. * IMPACTS...Coastal erosion and flooding of low lying areas is likely. * ADDITIONAL DETAILS...Gale force southerly winds will lead to high water levels along the Kuskokwim Delta coast during the Monday afternoon high tide. Half an inch to 1.25 inches of rainfall are also forecast for the area through Monday afternoon, which may fill low-lying areas that normally take on water during lower level coastal flooding events, resulting in higher than normal water levels in addition to the onshore surge. Water levels decrease Monday evening with a receding tide and diminishing southerly winds.

INSTRUCTION: A coastal flood advisory indicates that onshore winds and tides will combine to generate flooding of low areas along the shore.

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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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