Weather Alert in New Mexico
Wind Advisory issued February 18 at 5:13AM MST until February 19 at 5:00AM MST by NWS Albuquerque NM
AREAS AFFECTED: Union County; Harding County; Eastern San Miguel County; Quay County; Curry County; De Baca County
DESCRIPTION: * WHAT...West winds 25 to 35 mph with gusts up to 55 mph expected. * WHERE...Curry County, De Baca County, Quay County, Eastern San Miguel County, Harding County, and Union County. * WHEN...From 11 AM this morning to 5 AM MST Thursday. * IMPACTS...Gusty winds will blow around unsecured objects. Tree limbs may be blown down. Expect strong crosswinds on area roadways. * ADDITIONAL DETAILS...Visibility may drop below three miles at times in blowing dust on the eastern plains.
INSTRUCTION: Take action to secure trash cans, lawn furniture, and other loose or lightweight outdoor objects. Dangerous driving conditions can be expected, especially for motorists in high profile vehicles and during periods of dense blowing dust.
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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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