Weather Alert in New Mexico
High Wind Watch issued February 14 at 10:41PM MST until February 17 at 8:00PM MST by NWS Albuquerque NM
AREAS AFFECTED: Northern Sangre de Cristo Mountains; Southern Sangre de Cristo Mountains; East Slopes Sangre de Cristo Mountains; Central Highlands; South Central Mountains; Northeast Highlands; Guadalupe County; Eastern Lincoln County; Southwest Chaves County
DESCRIPTION: * WHAT...West winds 30 to 40 mph with gusts up to 60 mph possible. * WHERE...Sangre de Cristo Mountains, Central Highlands, South Central Mountains, Northeast Highlands, Guadalupe County, Eastern Lincoln County, and Southwest Chaves County. * WHEN...From Tuesday morning through Tuesday evening. * IMPACTS...Damaging winds could blow down trees and power lines. Power outages are possible. Travel will be difficult, especially for high profile vehicles. * ADDITIONAL DETAILS...The Sangre de Cristo Mountains may receive a few inches of snow as well, with blowing snow resulting in significant reductions to visibility. Patchy blowing dust may develop in the highlands east of the central mountain chain.
INSTRUCTION: Monitor the latest forecasts and warnings for updates.
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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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