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 Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
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
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