Weather Alert in Alaska
Hydrologic Outlook issued August 24 at 1:17PM AKDT by NWS Anchorage AK
AREAS AFFECTED: Kuskokwim Valley West; Kuskokwim Valley East; Interior Kuskokwim Delta; Western Capes; Northern Bristol Bay Coast; Inland Bristol Bay
DESCRIPTION: ESFAFC Prolonged, widespread rainfall is expected across Southwest Alaska this week. Steadier rainfall, which can be moderate to heavy at times, is expected to begin Monday and last through at least Wednesday with showers lingering through the rest of the week. Widespread rainfall totals of 1.5 to 3 inches is expected with locally higher amounts possible. The highest rainfall totals of at least 2.5 to 4 inches is expected close to the mountains near Togiak and the Western Capes. Expect water levels to rise along small streams and rivers, especially in areas of steeper terrain.
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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