Weather Alert in Colorado
Fire Weather Watch issued March 31 at 8:59PM MDT until April 2 at 8:00PM MDT by NWS Goodland KS
AREAS AFFECTED: Yuma; Kit Carson County; Cheyenne; Wallace; Greeley; Wichita
DESCRIPTION: Winds from the south Thursday afternoon and early evening are forecast to be around 15-25 MPH sustained with gusts up to 35 MPH. RH values are currently forecast to dry into the low to mid teens as temperatures warm into the mid to upper 70s. * AFFECTED AREA...Fire Weather Zones 027 Wallace, 041 Greeley, 042 Wichita, 252 Yuma, 253 Kit Carson and 254 Cheyenne CO. * TIMING...From Thursday afternoon through Thursday evening. * WINDS...South 15 to 25 mph with gusts up to 35 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: 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 Precipitation?
Home - Education - Precipitation - Precipitation
Next Topic: Rain
Precipitation can refer to many different forms of water that
may fall from clouds. Precipitation occurs after a cloud has become saturated to
the point where its water particles are more dense than the air below the cloud.
In most cases, precipitation will reach the ground, but it is not uncommon for
precipitation to evaporate before it reaches the earth's surface.
When precipitation evaporates before it contacts the ground it is called Virga.
Graupel, hail, sleet, rain, drizzle, and snow are forms of precipitation, but fog
and mist are not considered precipitation because the water vapor which
constitutes them isn't dense enough to fall to the ground.
Next Topic: Rain
Weather Topic: What are Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
Next Topic: Sleet
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