Weather Alert in California
Wind Advisory issued March 30 at 10:06PM PDT until April 2 at 2:00AM PDT by NWS San Diego CA
AREAS AFFECTED: Coachella Valley; San Gorgonio Pass Near Banning
DESCRIPTION: * WHAT...West winds 20 to 30 mph with gusts to 60 mph, except locally to 70 mph near San Gorgonio Pass Monday and Tuesday. Most widespread winds will be Tuesday. * WHERE...Coachella Valley and San Gorgonio Pass near Banning. * WHEN...Until 2 AM PDT Wednesday. * IMPACTS...Gusty winds will blow around unsecured objects. Tree limbs could be blown down and a few power outages may result. Reduced visibility in blowing dust in the desrts. * ADDITIONAL DETAILS...Gusty winds will occur at times through Wednesday, especially during the afternoons and nights.
INSTRUCTION: Winds this strong can make driving difficult, especially for high profile vehicles. Use extra caution.
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Weather Topic: What are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
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
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