Weather Alert in Alaska
Special Weather Statement issued August 28 at 10:58PM AKDT by NWS Anchorage AK
AREAS AFFECTED: Southern Kachemak Bay; SW Kenai Peninsula; NW Kenai Peninsula
DESCRIPTION: Strong southwesterly winds will develop early Friday morning and continue into Friday afternoon in the wake of a frontal system moving east across the region. The strongest wind gusts will range between 30 and 45 mph, with the strongest gusts focused along the immediate coast from Anchor Point north to Nikiski. Other locations, including Homer, Soldotna, and Kenai could see gusts as high as 40 mph. Winds are then expected to diminish in intensity by Friday evening as the front continues to exit the region. People are urged to secure loose objects that could be blown around by the strong winds and use caution while traveling. Trees are still fully leafed and will be unusually vulnerable to damage from the strong winds. Localized power outages will be possible due the potential for strong winds to bring down tree branches onto power lines.
INSTRUCTION: N/A
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Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - 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
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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