Weather Alert in Kansas
Fire Weather Watch issued February 15 at 2:06AM CST until February 17 at 6:00PM CST by NWS Dodge City KS
AREAS AFFECTED: Ellis; Rush; Pawnee; Stafford; Edwards; Kiowa; Pratt; Comanche; Barber
DESCRIPTION: ...Critical Wildfire Danger Expected Tuesday Afternoon... The National Weather Service in Dodge City has issued a Fire Weather Watch for wind and low relative humidity, which is in effect Tuesday afternoon. * AFFECTED AREA...Fire Weather Zone 031 Ellis, Fire Weather Zone 046 Rush, Fire Weather Zone 065 Pawnee, Fire Weather Zone 066 Stafford, Fire Weather Zone 079 Edwards, Fire Weather Zone 080 Kiowa, Fire Weather Zone 081 Pratt, Fire Weather Zone 089 Comanche and Fire Weather Zone 090 Barber. * TIMING...Tuesday afternoon. * WINDS...Southwest 35 to 45 mph with gusts up to 55 mph. * RELATIVE HUMIDITY...As low as 15 percent. * IMPACTS...Any ignitions will have the potential to become wildfires quickly, and spread rapidly. Outdoor burning is strongly discouraged.
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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