Weather Alert in Colorado
Avalanche Watch issued February 10 at 4:38PM MST by NWS Denver CO
AREAS AFFECTED: Elkhead and Park Mountains; West Elk and Sawatch Mountains; Flat Tops; West Jackson and West Grand Counties Above 9000 Feet
DESCRIPTION: AVABOU THE FOLLOWING MESSAGE IS TRANSMITTED AT THE REQUEST OF THE COLORADO AVALANCHE INFORMATION CENTER. AVALANCHE WATCH IN EFFECT FROM 5:00 PM TUESDAY UNTIL 5:00 PM WEDNESDAY *WHAT Dangerous avalanche conditions are taking shape. Expect the Avalanche Danger to rise to HIGH (Level 4 of 5) by late Wednesday evening. *WHERE Park Range, Flat Tops, Elk heads, and Ruby Raggeds *WHEN Expect dangerous avalanche conditions to begin overnight Wednesday and last through Thursday. *IMPACTS Heavy snow and wind, drifting snow, will create dangerous avalanche conditions. Large and dangerous avalanches will be easy to trigger once the new snow accumulates. Avalanches will run naturally. *PRECAUTION/PREPAREDNESS ACTIONS Travel in backcountry avalanche terrain is not recommended on THURSDAY. Avoid travel on and under slopes with a slope angle steeper than about 30 degrees. You can find more detailed information at colorado.gov/avalanche Davis
INSTRUCTION: N/A
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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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