Weather Alert in Colorado
Winter Storm Warning issued February 15 at 11:56AM MST until February 18 at 11:00PM MST by NWS Pueblo CO
AREAS AFFECTED: Eastern Sawatch Mountains above 11000 Ft; Eastern San Juan Mountains Above 10000 Ft
DESCRIPTION: * WHAT...Heavy wind driven snow expected. Total snow accumulations between 8 and 14 inches. Up to 21 inches possible across portions of the Eastern San Juan Mountains. Winds gusting as high as 80 mph causing blowing and drifting snow. * WHERE...Eastern Sawatch Mountains Above 11000 Feet and Eastern San Juan Mountains Above 10000 Feet. * WHEN...From 11 PM Monday to 11 PM MST Wednesday. * IMPACTS...Travel could be very difficult to impossible. Widespread blowing snow could significantly reduce visibility. Very strong winds could cause power outages and tree damage. * ADDITIONAL DETAILS...The heaviest snow will fall late Monday night through Tuesday morning with another round of heavy snow on Wednesday. Strong winds and blowing snow will continue throughout the period.
INSTRUCTION: If you must travel, keep an extra flashlight, food, and water in your vehicle in case of an emergency. 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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