Weather Alert in Colorado
Fire Weather Watch issued February 14 at 12:46AM MST until February 17 at 8:00PM MST by NWS Goodland KS
AREAS AFFECTED: Cheyenne
DESCRIPTION: For Sunday, southwest winds of 15-20 mph are forecast to begin around around 8-9 am Mountain time across Yuma and Kit Carson county before expanding east into the remainder of the Fire Weather Watch through the afternoon. For Tuesday, low relative humidity and sustained winds around 40 mph could lead to explosive fire growth for fires that ignite. Southwest winds could change to west behind a cold front in the afternoon. * AFFECTED AREA...Fire Weather Zone 254 Cheyenne. * TIMING...From Tuesday morning through Tuesday evening. * WINDS...For Sunday, southwest winds of 15-20 mph gusting to 35 mph. For Tuesday, southwest 35 to 45 mph with gusts up to 65 mph. West 35 to 45 mph with gusts up to 60 mph. * RELATIVE HUMIDITY...As low as 12 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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North America Water Vapor (Moisture)
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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
Weather Topic: What are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
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