Weather Alert in California
Winter Storm Watch issued February 16 at 10:06AM PST until February 18 at 4:00AM PST by NWS Las Vegas NV
AREAS AFFECTED: Owens Valley
DESCRIPTION: * WHAT...Heavy snow possible. Total snow accumulations of 3 to 6 inches, mainly north of Lone Pine. Winds could gust as high as 40 mph. * WHERE...Owens Valley. * WHEN...From Tuesday morning through late-Tuesday night. * IMPACTS...Slick and snow-covered roadways will quickly become dangerous with numerous slide-offs and spin-outs possible. * ADDITIONAL DETAILS...Snowfall is expected to develop by Tuesday afternoon with snow levels hovering near the valley floor. Cooler air will move in after dark with increasing snow intensity expected, which will worsen roadway conditions.
INSTRUCTION: Persons should delay all travel if possible. If travel is absolutely necessary, drive with extreme caution and be prepared for sudden changes in visibility. Leave plenty of room between you and the motorist ahead of you, and allow extra time to reach your destination. Avoid sudden braking or acceleration, and be especially cautious on hills or when making turns. Make sure your car is winterized and in good working order.
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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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