Weather Alert in New Mexico
Winter Weather Advisory issued February 18 at 11:21AM MST until February 18 at 11:00PM MST by NWS Albuquerque NM
AREAS AFFECTED: Northern Sangre de Cristo Mountains; Southern Sangre de Cristo Mountains
DESCRIPTION: * WHAT...Snow expected. Total snow accumulations between 1 and 4 inches, except up to 8 inches over high mountain peaks. Winds gusting as high as 65 mph. * WHERE...Northern and Southern Sangre de Cristo Mountains. * WHEN...Until 11 PM MST this evening. * IMPACTS...Travel could be very difficult. Tire traction will be reduced. Extend the distance between your vehicle and the vehicle in front of you. Areas of blowing snow could significantly reduce visibility. Very strong winds could cause extensive damage to trees and power lines. * ADDITIONAL DETAILS...A cold front will cross from the northwest, bring a few snow showers across the mountains during the evening and into the nighttime hours. Visibility will drop below a half mile at times during periods of snow and blowing snow.
INSTRUCTION: Slow down and use caution while traveling. For the latest road conditions, dial 511 or 1.800.432.4269, or visit http://nmroads.com.
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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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