Weather Alert in New Mexico
Winter Weather Advisory issued February 13 at 11:28AM MST until February 14 at 5:00AM MST by NWS Albuquerque NM
AREAS AFFECTED: Tusas Mountains Including Chama; Northern Sangre de Cristo Mountains; Southern Sangre de Cristo Mountains
DESCRIPTION: * WHAT...Snow expected. Total snow accumulations between 4 and 8 inches above 8,500ft with lesser amounts below. * WHERE...Northern and Southern Sangre de Cristo Mountains, and Tusas Mountains Including Chama. * WHEN...Until 5 AM MST Saturday. * IMPACTS...High mountain roads and passes will likely become slick and hazardous. Travel could be very difficult. Tire traction will be reduced. Extend the distance between your vehicle and the vehicle in front of you.
INSTRUCTION: Slow down and use caution while traveling. For the latest road conditions, dial 511 or 1.800.432.4269, or visit http://nmroads.com.
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Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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