Weather Alert in Colorado

Recent Locations: Clements, CA   New Windsor, NY   Denver, CO  

Fire Weather Watch issued March 31 at 8:59PM MDT until April 2 at 8:00PM MDT by NWS Goodland KS

AREAS AFFECTED: Yuma; Kit Carson County; Cheyenne; Wallace; Greeley; Wichita

DESCRIPTION: Winds from the south Thursday afternoon and early evening are forecast to be around 15-25 MPH sustained with gusts up to 35 MPH. RH values are currently forecast to dry into the low to mid teens as temperatures warm into the mid to upper 70s. * AFFECTED AREA...Fire Weather Zones 027 Wallace, 041 Greeley, 042 Wichita, 252 Yuma, 253 Kit Carson and 254 Cheyenne CO. * TIMING...From Thursday afternoon through Thursday evening. * WINDS...South 15 to 25 mph with gusts up to 35 mph. * RELATIVE HUMIDITY...As low as 13 percent. * IMPACTS...Unpredictable fire behavior. Any fires that develop may rapidly grow and spread out of control.

INSTRUCTION: A Fire Weather Watch means that critical fire weather conditions are forecast to occur. Listen for later forecasts and possible red flag warnings.

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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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