Weather Alert in Hawaii
Flood Advisory issued February 8 at 9:13AM HST until February 8 at 12:15PM HST by NWS Honolulu HI
AREAS AFFECTED: Maui, HI
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall. * WHERE...The island of Molokai in Maui County. * WHEN...Until 1215 PM HST. * IMPACTS...Minor flooding on roads, poor drainage areas, and in streams. Some low-water crossings may become impassable. River or stream flows are elevated. * ADDITIONAL DETAILS... - At 909 AM HST, radar indicated heavy rain falling over eastern portions of Molokai. Rain was falling at a rate of 1 to 2 inches per hour, with the heaviest rain occurring between Kalawao and Halawa Valley. - Some locations that will experience flooding include... Kamalo, Ualapue, Kalaupapa National Park, Pukoo, Kawela, Halawa Valley, Kaunakakai and Kualapuu.
INSTRUCTION: Stay away from streams, drainage ditches and low lying areas prone to flooding. A Flood Watch is also in effect until 6 PM HST Monday.
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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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