Weather Alert in Kansas
Fire Weather Watch issued February 15 at 12:37AM MST until February 17 at 8:00PM MST by NWS Goodland KS
AREAS AFFECTED: Norton; Sheridan; Graham; Gove; Wichita
DESCRIPTION: For Sunday, southwest winds of 15-25 mph are forecast to begin around 8-9 am Mountain time across Yuma and Kit Carson county before expanding east into the remainder of the Red Flag Warning For Tuesday, low relative humidity and sustained winds around 40 mph could lead to extreme fire spread for any fires that ignite. Southwest winds could change to west behind a cold front in the afternoon. The National Weather Service in Goodland has issued a Fire Weather Watch for wind and low relative humidity, which is in effect from Tuesday afternoon through Tuesday evening. * AFFECTED AREA...Fire Weather Zones 004 Norton, 015 Sheridan, 016 Graham, 029 Gove and 042 Wichita. * TIMING...From Tuesday afternoon through Tuesday evening. * WINDS...For Sunday, southwesterly winds of 15 to 25 mph gusting up to 30 mph. For Tuesday, West 25 to 35 mph with gusts up to 60 mph. * RELATIVE HUMIDITY...As low as 13 percent. * IMPACTS...Dangerous and 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 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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