Weather Alert in New Mexico
Dust Storm Warning issued June 30 at 6:11PM MDT until June 30 at 8:15PM MDT by NWS El Paso Tx/Santa Teresa NM
AREAS AFFECTED: Hidalgo, NM
DESCRIPTION: The National Weather Service in El Paso has issued a * Dust Storm Warning for... West central Hidalgo County in southwestern New Mexico... * Until 815 PM MDT. * At 609 PM MDT, blowing dust is expected for I-10 between AZ/NM state line and Hidalgo/Grant County lines. This warning includes all of I-10 between MM 1 to MM 33. HAZARD...Less than a quarter mile visibility with strong winds up to 40 to 50 mph. SOURCE...Department of Transportation Officials. IMPACT...Dangerous life-threatening travel. * This includes Interstate 10 in New Mexico between mile markers 1 and 33. Locations impacted include... Steins, Lordsburg, Road Forks, Lordsburg Playa, Pyramid Mountains, and Shakespeare.
INSTRUCTION: Dust storms lead to dangerous driving conditions with visibility reduced to near zero. If driving, avoid dust storms if possible. If caught in one, pull off the road, turn off your lights and keep your foot off the brake.
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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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