Weather Alert in Colorado
Red Flag Warning issued February 25 at 5:39AM MST until February 25 at 7:00PM MST by NWS Goodland KS
AREAS AFFECTED: Yuma; Kit Carson County; Cheyenne; Cheyenne; Sherman; Dundy; Hitchcock; Red Willow
DESCRIPTION: Strong westerly winds will spread over the plains of Colorado and adjacent areas Wednesday late Wednesday through the afternoon. Strong winds, combined with very dry fuels will promote the potential for rapid to extreme fire spread. The strongest winds are forecast across Yuma county through the mid afternoon before spreading east through the rest of the afternoon. A strong cold front is expected to sweep across the area around during the mid to late afternoon, shifting winds to the north- northwest making any ongoing fire control efforts difficult. High based showers and isolated storms may pose a dry lightning threat this afternoon as well along with gusty, erratic winds. * AFFECTED AREA...Fire Weather Zones 001 Cheyenne KS, 013 Sherman, 079 Dundy, 080 Hitchcock, 081 Red Willow, 252 Yuma, 253 Kit Carson and 254 Cheyenne CO. * TIMING...From 11 AM MST /noon CST/ this morning to 7 PM MST /8 PM CST/ this evening. * WINDS...Northwest 25 to 35 mph with gusts up to 55 mph. * RELATIVE HUMIDITY...Around 17 percent. * LIGHTNING...Isolated dry storms possible. Little rainfall amounts expected. * 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 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
Weather Topic: What is Snow?
Home - Education - Precipitation - Snow
Next Topic: Stratocumulus Clouds
Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake,
has unique characteristics, but all of them grow in a hexagonal structure.
Snowfall can last for sustained periods of time and result in significant buildup
of snow on the ground.
On the earth's surface, snow starts out light and powdery, but as it begins to melt
it tends to become more granular, producing small bits of ice which have the consistency of
sand. After several cycles of melting and freezing, snow can become very dense
and ice-like, commonly known as snow pack.
Next Topic: Stratocumulus Clouds
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