Weather Alert in Colorado

Recent Locations: Eads, CO  
Current Alerts for Eads, CO: High Wind Warning

High Wind Warning issued March 14 at 6:40PM MDT until March 15 at 8:00PM MDT by NWS Goodland KS

AREAS AFFECTED: Yuma County; Kit Carson County; Cheyenne County; Cheyenne; Rawlins; Decatur; Norton; Sherman; Thomas; Sheridan; Graham; Wallace; Logan; Gove; Greeley; Wichita; Dundy; Hitchcock; Red Willow

DESCRIPTION: * WHAT...North winds 35 to 45 mph with gusts up to 70 mph expected. * WHERE...Portions of east central and northeast Colorado, northwest and west central Kansas and southwest Nebraska. * WHEN...From midnight MDT /1 AM CDT/ tonight to 8 PM MDT /9 PM CDT/ Sunday. Peak wind gusts are expected between 9 AM and 3 PM MDT. * IMPACTS...High winds may move loose debris, damage property and cause power outages. Travel will be difficult especially for high profile vehicles. Plumes of dust with visibilities under a mile downwind of loose soil.

INSTRUCTION: People are urged to secure loose objects that could be blown around or damaged by the wind.

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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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