Weather Alert in New Mexico
High Wind Warning issued February 18 at 5:13AM MST until February 19 at 5:00AM MST by NWS Albuquerque NM
AREAS AFFECTED: Glorieta Mesa Including Glorieta Pass; Northern Sangre de Cristo Mountains; Southern Sangre de Cristo Mountains; East Slopes Sangre de Cristo Mountains; Central Highlands; South Central Mountains; Johnson and Bartlett Mesas Including Raton Pass; Far Northeast Highlands; Northeast Highlands; Guadalupe County; Eastern Lincoln County; Southwest Chaves County
DESCRIPTION: * WHAT...West winds 30 to 40 mph with gusts up to 60 mph expected. * WHERE...Portions of central, east central, north central, northeast, and southeast New Mexico along and just east of the central mountain chain, as well as Guadalupe County. * WHEN...From 11 AM this morning to 5 AM MST Thursday. * IMPACTS...Damaging winds could blow down trees and power lines. Power outages are possible. Travel will be difficult, especially for high profile vehicles. * ADDITIONAL DETAILS...A few inches of snow are forecast in the Sangre de Cristo Mountains this afternoon. Periods of snow and blowing snow will drop visibility below a half mile at times. Snow drifts will reach over 6 inches in spots.
INSTRUCTION: Take action to secure trash cans, lawn furniture, and other loose or lightweight outdoor objects. Dangerous driving conditions can be expected, especially for motorists in high profile vehicles.
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Weather Topic: What are Cirrus Clouds?
Home - Education - Cloud Types - Cirrus Clouds
Next Topic: Condensation
Cirrus clouds are high-level clouds that occur above 20,000 feet
and are composed mainly of ice crystals.
They are thin and wispy in appearance.
What do they indicate?
They are often the first sign of an approaching storm.
Next Topic: Condensation
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
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