Weather Alert in Colorado
Red Flag Warning issued February 18 at 8:32AM MST until February 18 at 5:00PM MST by NWS Goodland KS
AREAS AFFECTED: Kit Carson County; Cheyenne; Wallace; Logan; Gove; Greeley; Wichita
DESCRIPTION: Critical fire weather conditions are forecast again Wednesday for portions of the area. Winds are forecast to be from the southwest with wind gusts around 45 mph. Strongest winds are favoring Cheyenne county Colorado and Greeley county Kansas. Winds are forecast to increase around 10-11am mountain time. Be aware of shifting winds to the northwest early Thursday morning with a cold front with strong winds possible. * AFFECTED AREA...Fire Weather Zones 027 Wallace, 028 Logan, 029 Gove, 041 Greeley, 042 Wichita, 253 Kit Carson and 254 Cheyenne. * TIMING...Until 5 PM MST /6 PM CST/ this afternoon. * WINDS...Southwest 15 to 25 mph with gusts up to 45 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: Comply with burn bans and regulations. Avoid driving on dry grass or brush. Maintain vehicle brakes and tires and secure tow chains to avoid dragging. Never toss lit cigarettes onto the ground.
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Weather Topic: What is Evaporation?
Home - Education - Precipitation - Evaporation
Next Topic: Fog
Evaporation is the process which returns water from the earth
back to the atmosphere, and is another crucial process in the water cycle.
Evaporation is the transformation of liquid into gas, and it happens because
molecules are excited by the application of energy and turn into vapor.
In order for water to evaporate it has to be on the surface of a body of water.
Next Topic: Fog
Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
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