Weather Alert in California
Winter Weather Advisory issued March 13 at 12:08PM PDT until March 14 at 11:00AM PDT by NWS Medford OR
AREAS AFFECTED: Central Siskiyou County
DESCRIPTION: * WHAT...Snow expected. Total snow accumulations of one half to 3 inches in the lower elevation valley areas from Yreka to Gazelle, but 3 to 6 inches near Hilt and around Weed. Winds gusting as high as 55 mph. * WHERE...Central Siskiyou County County, including I-5 from Hilt south to Weed. * WHEN...From 2 AM to 11 AM PDT Friday. * IMPACTS...Plan on slippery road conditions. The hazardous conditions could impact the Friday morning commute. Strong winds could cause tree damage and blowing snow.
INSTRUCTION: Slow down and use caution while traveling. Call 511 or visit quickmap.dot.ca.gov 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
