Weather Alert in Utah
Winter Weather Advisory issued February 16 at 11:31AM MST until February 19 at 5:00AM MST by NWS Grand Junction CO
AREAS AFFECTED: La Sal and Abajo Mountains
DESCRIPTION: * WHAT...Snow expected above 8000 feet. Total snow accumulations between 6 and 12 inches. Winds gusting as high as 65 mph. * WHERE...La Sal and Abajo Mountains. * WHEN...From 11 PM this evening to 5 AM MST Thursday. * IMPACTS...Travel could be very difficult. Blowing snow may result in near zero visibility at times. The hazardous conditions could impact the Tuesday morning and evening commutes. Strong winds could cause tree damage.
INSTRUCTION: Slow down and use caution while traveling. The latest road conditions for the state you are calling from can be obtained by calling 5 1 1.
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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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