Weather Alert in New Mexico
Wind Advisory issued February 16 at 11:33AM MST until February 17 at 8:00PM MST by NWS Albuquerque NM
AREAS AFFECTED: West Central Highlands; Southwest Mountains; Jemez Mountains; Upper Rio Grande Valley; Espanola Valley; Santa Fe Metro Area; Middle Rio Grande Valley/Albuquerque Metro Area; Lower Rio Grande Valley; Sandia/Manzano Mountains Including Edgewood; Estancia Valley; South Central Highlands; Upper Tularosa Valley
DESCRIPTION: * WHAT...West winds 30 to 40 mph with gusts up to 55 mph expected. * WHERE...Portions of central, north central, and west central New Mexico, including the Albuquerque and Santa Fe Metro areas. * WHEN...From 8 AM to 8 PM MST Tuesday. * IMPACTS...Gusty winds will blow around unsecured objects. Tree limbs may be blown down. Expect strong crosswinds on area roadways. * ADDITIONAL DETAILS...Patchy blowing dust may develop due to the strong winds and dry antecedent conditions. Visibility may be reduced to less than three miles in localized areas.
INSTRUCTION: Winds this strong can make driving difficult, especially for high profile vehicles. Use extra caution.
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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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