Weather Alert in New Mexico
Winter Storm Warning issued February 17 at 5:18AM MST until February 17 at 8:00PM MST by NWS Albuquerque NM
AREAS AFFECTED: Tusas Mountains Including Chama
DESCRIPTION: * WHAT...Heavy snow expected. Total snow accumulations of 4 to 8 inches above 8000 feet and up to 4 inches below 8000 feet. Winds gusting as high as 60 mph. * WHERE...Tusas Mountains Including Chama. * WHEN...Until 8 PM MST this evening. * IMPACTS...Visibilities may drop below 1/4 mile due to falling and blowing snow. Periods of whiteout conditions will make travel treacherous. Strong winds could cause extensive damage to trees and power lines. * ADDITIONAL DETAILS...Snow drifts will reach over 2 feet deep in spots.
INSTRUCTION: If you must travel, keep an extra flashlight, food, and water in your vehicle in case of an emergency. For the latest road conditions, dial 511 or 1.800.432.4269, or visit http://nmroads.com.
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Weather Topic: What is Precipitation?
Home - Education - Precipitation - Precipitation
Next Topic: Rain
Precipitation can refer to many different forms of water that
may fall from clouds. Precipitation occurs after a cloud has become saturated to
the point where its water particles are more dense than the air below the cloud.
In most cases, precipitation will reach the ground, but it is not uncommon for
precipitation to evaporate before it reaches the earth's surface.
When precipitation evaporates before it contacts the ground it is called Virga.
Graupel, hail, sleet, rain, drizzle, and snow are forms of precipitation, but fog
and mist are not considered precipitation because the water vapor which
constitutes them isn't dense enough to fall to the ground.
Next Topic: Rain
Weather Topic: What are Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
Next Topic: Sleet
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