Weather Alert in Colorado
Fire Weather Watch issued February 15 at 5:14PM MST until February 16 at 6:00PM MST by NWS Denver CO
AREAS AFFECTED: North Douglas County Below 6000 Feet/Denver/West Adams and Arapahoe Counties/East Broomfield County; Morgan County
DESCRIPTION: ...PROLONGED PERIOD OF CRITICAL FIRE WEATHER CONDITIONS THROUGH AT LEAST TUESDAY... ...EXTREMELY CRITICAL FIRE WEATHER CONDITIONS REMAIN POSSIBLE TUESDAY... .Recent dry conditions combining with above normal temperatures and periods of gusty winds will bring potentially critical fire weather conditions again on Monday. Stronger, more widespread westerly winds are expected to develop Tuesday, possibly producing extremely critical fire weather conditions with wind gusts as high as 65 mph across the plains. ...FIRE WEATHER WATCH REMAINS IN EFFECT FROM TUESDAY MORNING THROUGH TUESDAY EVENING FOR WIND AND LOW RELATIVE HUMIDITY FOR THE DENVER METRO AND MORGAN COUNTY... * AFFECTED AREA...Fire Weather Zones 240 and 244. * TIMING...For the first Fire Weather Watch, from Monday morning through Monday afternoon. For the second Fire Weather Watch, from Tuesday morning through Tuesday evening. * WINDS...Southwest winds 5 to 15 mph with gusts up to 25 mph on Monday. West winds 30 to 40 mph with gusts up to 60 mph on Tuesday. * RELATIVE HUMIDITY...As low as 11 percent. * IMPACTS...Conditions will be favorable for rapid fire spread. Avoid outdoor burning and any activity that may produce a spark and start a wildfire.
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
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
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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