Weather Alert in Colorado
Winter Weather Advisory issued February 15 at 7:37PM MST until February 18 at 11:00PM MST by NWS Pueblo CO
AREAS AFFECTED: Western Mosquito Range/East Lake County Above 11000 Ft; Leadville Vicinity/Lake County Below 11000 Ft; Western Chaffee County Between 9000 and 11000 Ft; La Garita Mountains Above 10000 Ft; Upper Rio Grande Valley/Eastern San Juan Mountains Below 10000 Ft
DESCRIPTION: * WHAT...Snow expected. Total snow accumulations between 4 and 12 inches. Winds gusting as high as 75 mph across the higher peaks and lower east facing slopes at times. * WHERE...La Garita Mountains Above 10000 Feet, Central Lake County Below 11000 Feet, Western Chaffee County Between 9000 and 11000 Feet, Western Mosquito Range Above 11000 Feet, and Upper Rio Grande Valley and San Juan Mountains Below 10000 Feet. * WHEN...From 11 PM Monday to 11 PM MST Wednesday. * IMPACTS...Travel could be very difficult to impossible. Very strong winds could cause power outages and tree damage.
INSTRUCTION: Slow down and use caution while traveling. The latest road conditions for the state you are calling from can be obtained by calling 5 1 1.
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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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