Weather Alert in California
Winter Weather Advisory issued February 17 at 8:20PM PST until February 18 at 4:00AM PST by NWS Las Vegas NV
AREAS AFFECTED: Owens Valley
DESCRIPTION: * WHAT...Snow expected. Total snow accumulations of 4 to 8 inches around Bishop. Winds could gust as high as 40 mph. Accumulations of 2 to 4 inches possible along the US-395 corridor south of Bishop late tonight mainly above 4000 feet. * WHERE...Owens Valley. * WHEN...Until 4 AM PST Wednesday. * IMPACTS...Plan on slippery road conditions. Gusty winds could bring down tree branches. * ADDITIONAL DETAILS...Periods of heavy snow will continue this evening before tapering off late tonight. Heaviest snow has been in the Bishop area but additional snow accumulations will spread south overnight.
INSTRUCTION: Slow down and use caution while traveling. Call 1-800-427-7623 for road information.
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Weather Topic: What is Evaporation?
Home - Education - Precipitation - Evaporation
Next Topic: Fog
Evaporation is the process which returns water from the earth
back to the atmosphere, and is another crucial process in the water cycle.
Evaporation is the transformation of liquid into gas, and it happens because
molecules are excited by the application of energy and turn into vapor.
In order for water to evaporate it has to be on the surface of a body of water.
Next Topic: Fog
Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
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