Weather Alert in Nevada
Hydrologic Outlook issued August 23 at 11:56PM PDT by NWS Elko NV
AREAS AFFECTED: Elko, NV; Eureka, NV
DESCRIPTION: ESFLKN Deep, monsoonal moisture will surge northward into most of Northern and Central Nevada this afternoon through Wednesday evening. As a result, showers and thunderstorms will develop across much of Northern and Central Nevada each afternoon and evening today through Wednesday. Slow storm motions may produce heavy rainfall and localized flooding. Of particular concern are recent, large burn scars, including the Snowstorm Complex near Midas, the Cottonwood Peak fire north of Tuscarora, the Hot Canyon fire northwest of Montello, and the Adobe fire north of Elko. Numerous smaller burn scars from this fire season also remain vulnerable. Residents near recent burned scars should have multiple ways to receive Flash Flood Warnings and be prepared to act quickly. Travelers and recreationists should also remain alert and consider alternate plans.
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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