Weather Alert in Colorado
Winter Storm Warning issued February 15 at 7:37PM 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 Contrails?
Home - Education - Cloud Types - Contrails
Next Topic: Cumulonimbus Clouds
A contrail is an artificial cloud, created by the passing of an
aircraft.
Contrails form because water vapor in the exhaust of aircraft engines is suspended
in the air under certain temperatures and humidity conditions. These contrails
are called exhaust contrails.
Another type of contrail can form due to a temporary reduction in air pressure
moving over the plane's surface, causing condensation.
These are called aerodynamic contrails.
When you can see your breath on a cold day, it is also because of condensation.
The reason contrails last longer than the condensation from your breath is
because the water in contrails freezes into ice particles.
Next Topic: Cumulonimbus Clouds
Weather Topic: What are Cumulus Clouds?
Home - Education - Cloud Types - Cumulus Clouds
Next Topic: Drizzle
Cumulus clouds are fluffy and textured with rounded tops, and
may have flat bottoms. The border of a cumulus cloud
is clearly defined, and can have the appearance of cotton or cauliflower.
Cumulus clouds form at low altitudes (rarely above 2 km) but can grow very tall,
becoming cumulus congestus and possibly the even taller cumulonimbus clouds.
When cumulus clouds become taller, they have a greater chance of producing precipitation.
Next Topic: Drizzle
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