Weather Alert in California
Winter Weather Advisory issued February 19 at 6:42AM PST until February 19 at 7:00PM PST by NWS Las Vegas NV
AREAS AFFECTED: Eastern Sierra Slopes of Inyo County
DESCRIPTION: * WHAT...Additional snow expected. Total snow accumulations between 8 and 14 inches above 8000 feet and between 4 and 8 inches above 6000 feet. Winds gusting as high as 60 mph. * WHERE...Eastern Sierra Slopes. * WHEN...Until 7 PM PST this evening. * IMPACTS...Roads will likely become slick and hazardous. Reduced visibility from blowing snow is possible and could make travel hazardous. Travel could be very difficult along State Route 168 to Aspendell. Strong winds could cause tree or power line damage.
INSTRUCTION: Slow down and use caution while traveling. Call 1-800-427-7623 for road information.
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North America Water Vapor (Moisture)
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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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