Weather Alert in California
Wind Advisory issued May 3 at 3:18AM PDT until May 4 at 4:00AM PDT by NWS Los Angeles/Oxnard CA
AREAS AFFECTED: San Luis Obispo County Inland Central Coast; Santa Lucia Mountains; Southern Salinas Valley; San Luis Obispo County Interior Valleys; Santa Ynez Valley
DESCRIPTION: * WHAT...Northwest winds 15 to 25 mph with gusts to 40 mph expected. Isolated gusts to 50 mph in the hills possible. * WHERE...San Luis Obispo County Inland Central Coast, San Luis Obispo County Interior Valleys, Santa Lucia Mountains, Santa Ynez Valley, and Southern Salinas Valley. * WHEN...From 3 PM this afternoon to 4 AM PDT Sunday. * IMPACTS...Gusty winds will blow around unsecured objects. Tree limbs could be blown down and a few power outages may result. Hazardous driving conditions, especially for big rigs and motor homes.
INSTRUCTION: Use extra caution on the roads. Secure loose objects.
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Weather Topic: What is Precipitation?
Home - Education - Precipitation - Precipitation
Next Topic: Rain
Precipitation can refer to many different forms of water that
may fall from clouds. Precipitation occurs after a cloud has become saturated to
the point where its water particles are more dense than the air below the cloud.
In most cases, precipitation will reach the ground, but it is not uncommon for
precipitation to evaporate before it reaches the earth's surface.
When precipitation evaporates before it contacts the ground it is called Virga.
Graupel, hail, sleet, rain, drizzle, and snow are forms of precipitation, but fog
and mist are not considered precipitation because the water vapor which
constitutes them isn't dense enough to fall to the ground.
Next Topic: Rain
Weather Topic: What are Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
Next Topic: Sleet
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