Weather Alert in Colorado
Winter Weather Advisory issued February 17 at 1:49PM 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. Additional snow accumulations between 4 and 12 inches, with locally higher amounts possible across the crest of the Sawatch range. Winds gusting as high as 60 mph. * WHERE...La Garita Mountains Above 10000 Feet, 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 Eastern San Juan Mountains Below 10000 Feet. * WHEN...Until 11 PM MST Wednesday. * IMPACTS...Travel could be very difficult to impossible. Very strong winds could cause power outages and tree damage. * ADDITIONAL DETAILS...Another round of heavy snow is expected for Wednesday.
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 Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
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