Weather Alert in Colorado
Winter Storm Warning issued February 17 at 8:25AM 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 16 inches. Up to 24 inches possible across portions of the Eastern San Juan Mountains. Winds gusting as high as 70 mph causing blowing and drifting snow and near zero visibility. * WHERE...Eastern Sawatch Mountains Above 11000 Feet and Eastern San Juan Mountains Above 10000 Feet. * WHEN...Until 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 through this 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 is Snow?
Home - Education - Precipitation - Snow
Next Topic: Stratocumulus Clouds
Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake,
has unique characteristics, but all of them grow in a hexagonal structure.
Snowfall can last for sustained periods of time and result in significant buildup
of snow on the ground.
On the earth's surface, snow starts out light and powdery, but as it begins to melt
it tends to become more granular, producing small bits of ice which have the consistency of
sand. After several cycles of melting and freezing, snow can become very dense
and ice-like, commonly known as snow pack.
Next Topic: Stratocumulus Clouds
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
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