Weather Alert in New Mexico
Winter Storm Watch issued February 16 at 12:01AM MST until February 17 at 8:00PM MST by NWS Albuquerque NM
AREAS AFFECTED: Northern Sangre de Cristo Mountains; Southern Sangre de Cristo Mountains
DESCRIPTION: * WHAT...Heavy snow possible. Total snow accumulations up to 5 inches possible. Winds could gust as high as 70 mph. * WHERE...Northern and Southern Sangre de Cristo Mountains. * WHEN...From late Monday night through Tuesday evening. * IMPACTS...Visibilities may drop below 1/4 mile due to falling and blowing snow. Whiteout conditions are possible and may make travel treacherous. Extend the distance between your vehicle and the vehicle in front of you. Strong winds could cause extensive damage to trees and power lines.
INSTRUCTION: Monitor the latest forecasts for updates on this situation.
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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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