Weather Alert in Colorado
Fire Weather Watch issued February 14 at 9:48PM MST until February 16 at 6:00PM MST by NWS Denver CO
AREAS AFFECTED: Jefferson and West Douglas Counties Above 6000 Feet/Gilpin/Clear Creek/Northeast Park Counties Below 9000 Feet; North Douglas County Below 6000 Feet/Denver/West Adams and Arapahoe Counties/East Broomfield County; Elbert/Central and East Douglas Counties Above 6000 Feet; Morgan County; Central and East Adams and Arapahoe Counties; Southeast Elbert County Below 6000 Feet/South Lincoln County
DESCRIPTION: ...PROLONGED PERIOD OF CRITICAL FIRE WEATHER CONDITIONS SUNDAY THROUGH MID NEXT WEEK... ...EXTREMELY CRITICAL FIRE WEATHER CONDITIONS POSSIBLE TUESDAY... .Recent dry conditions combining with above normal temperatures and periods of gusty winds will bring potentially critical fire weather conditions Sunday and Monday to parts of the eastern Colorado Plains. Stronger, more widespread westerly winds are expected to develop Tuesday, possibly producing extremely critical fire weather conditions with wind gusts as high as 65 mph across the plains. * AFFECTED AREA...Fire Weather Zones 216, 240, 241, 244, 245 and 247. * TIMING...For the first Fire Weather Watch, from Monday morning through Monday afternoon. For the second Fire Weather Watch, from Tuesday morning through Tuesday evening. * WINDS...Southwest winds 10 to 20 mph with gusts to 30 mph on Monday. West winds 30 to 40 mph with gusts up to 60 mph on Tuesday. * RELATIVE HUMIDITY...As low as 12 percent each afternoon. * IMPACTS...Conditions will be favorable for rapid fire spread. Avoid outdoor burning and any activity that may produce a spark and start a wildfire.
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 Sleet?
Home - Education - Precipitation - Sleet
Next Topic: Snow
Sleet is a form of precipitation in which small ice pellets are the primary
components. These ice pellets are smaller and more translucent than hailstones,
and harder than graupel. Sleet is caused by specific atmospheric conditions and
therefore typically doesn't last for extended periods of time.
The condition which leads to sleet formation requires a warmer body of air to be
wedged in between two sub-freezing bodies of air. When snow falls through a warmer
layer of air it melts, and as it falls through the next sub-freezing body of air
it freezes again, forming ice pellets known as sleet. In some cases, water
droplets don't have time to freeze before reaching the surface and the result is
freezing rain.
Next Topic: Snow
Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
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