Weather Alert in California
Wind Advisory issued May 3 at 2:32AM PDT until May 5 at 8:00PM PDT by NWS San Diego CA
AREAS AFFECTED: San Bernardino County Mountains; Apple and Lucerne Valleys
DESCRIPTION: * WHAT...Southwest winds 25 to 35 mph with gusts to 65 mph expected. Isolated gusts to 75 mph near the desert foothills of the mountains late Saturday night. * WHERE...San Bernardino County Mountains and Apple and Lucerne Valleys. * WHEN...From noon Saturday to 8 PM PDT Sunday. * IMPACTS...Gusty winds could blow around unsecured objects. Tree limbs could be blown down. * ADDITIONAL DETAILS...The strongest winds are expected Saturday night along the desert slopes of the mountains and Sunday afternoon for the Apple and Lucerne Valleys.
INSTRUCTION: Use extra caution when driving, especially if operating a high profile vehicle. Secure outdoor objects.
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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
