Weather Alert in California
Winter Weather Advisory issued April 1 at 12:12AM PDT until April 2 at 11:00AM PDT by NWS Medford OR
AREAS AFFECTED: Western Siskiyou County
DESCRIPTION: * WHAT...Snow expected above 4000 feet. Total snow accumulations 4 to 8 inches, except up to 14 inches above 5000 feet. Winds gusting as high as 40 mph over high and exposed terrain. * WHERE...Western Siskiyou County above 4000 feet. This also includes Etna Summit on Sawyers Bar Rd at 5950 ft. * WHEN...From 8 PM Wednesday to 11 AM PDT Thursday. * IMPACTS...Travel may be difficult. The hazardous conditions could impact the Thursday morning commute. Gusty winds could bring down tree branches. Gusty winds combined with snow may cause limited visibility. Use extra care if traveling through remote or isolated areas.
INSTRUCTION: Slow down and use caution while traveling. Call 511 or visit quickmap.dot.ca.gov for road information.
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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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