Weather Alert in Colorado
Special Weather Statement issued August 2 at 3:37PM MDT by NWS Denver CO
AREAS AFFECTED: North Douglas County Below 6000 Feet/Denver/West Adams and Arapahoe Counties/East Broomfield County; Central and South Weld County; Central and East Adams and Arapahoe Counties
DESCRIPTION: At 337 PM MDT, Doppler radar was tracking a line of strong thunderstorms extending from 5 miles southeast of Gilcrest to near Aurora, or extending from 14 miles south of Greeley to 12 miles east of Denver, moving east at 20 mph. HAZARD...Wind gusts of 50 to 55 mph. SOURCE...Radar indicated. IMPACT...Gusty winds could knock down tree limbs and blow around unsecured objects. Locations impacted include... Northeastern Denver, northeastern Aurora, eastern Commerce City, Brighton, Denver International Airport, D.I.A Terminal and Concourses, Fort Lupton, Lochbuie, Hudson, Keenesburg, Prospect Valley, Milton Reservoir and Roggen.
INSTRUCTION: Monitor the weather situation closely and be alert for threatening weather conditions. If on or near a lake|, get out of the water and secure loose items. Boaters can expect strong gusty winds and locally higher waves. Boaters should seek safe harbor immediately.
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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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