Weather Alert in New Mexico

Recent Locations: Merritt Island, FL   Uvalde, TX   Deming, NM  

High Wind Warning issued February 16 at 11:33AM MST until February 17 at 8:00PM MST by NWS Albuquerque NM

AREAS AFFECTED: Glorieta Mesa Including Glorieta Pass; East Slopes Sangre de Cristo Mountains; Central Highlands; South Central Mountains; Johnson and Bartlett Mesas Including Raton Pass; Far Northeast Highlands; Northeast Highlands; Union County; Harding County; Eastern San Miguel County; Guadalupe County; Quay County; Curry County; Roosevelt County; De Baca County; Chaves County Plains; Eastern Lincoln County; Southwest Chaves County

DESCRIPTION: * WHAT...Southwest to west winds 35 to 45 mph with gusts up to 70 mph expected. * WHERE...All of eastern New Mexico as well as the east slopes of the Sangre de Cristo Mountains, the Northeast and Central Highlands as well as the South Central Mountains. * WHEN...From 8 AM to 8 PM MST Tuesday. * 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...Patchy blowing dust may develop across the eastern plains due to the very strong west winds and dry antecedent conditions. Visibility may be reduced below one mile.

INSTRUCTION: Take action to secure trash cans, lawn furniture, and other loose or lightweight outdoor objects. Extremely hazardous driving conditions can be expected, especially for motorists in high profile vehicles who should consider delaying travel.

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Weather Topic: What are Contrails?

Home - Education - Cloud Types - Contrails

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

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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