Weather Alert in Colorado
Fire Weather Watch issued February 14 at 2:36AM MST until February 15 at 5:00PM MST by NWS Denver CO
AREAS AFFECTED: Sedgwick County; Phillips County
DESCRIPTION: ...PROLONGED PERIOD OF CRITICAL FIRE WEATHER CONDITIONS SUNDAY THROUGH MID NEXT WEEK... ...EXTREME FIRE WEATHER CONDITIONS POSSIBLE TUESDAY... .Recent dry conditions combining with above normal temperatures and pockets of gusty winds will bring potentially critical fire weather conditions Sunday and Monday to parts of the eastern Colorado Plains. Strong west winds are expected to develop Tuesday, possibly producing extreme fire weather conditions with widespread strong and gusty winds to 60 mph. ...FIRE WEATHER WATCH REMAINS IN EFFECT FROM TUESDAY MORNING THROUGH TUESDAY EVENING FOR WIND AND LOW RELATIVE HUMIDITY FOR SEDGWICK AND PHILLIPS COUNTIES... The National Weather Service in Denver has issued a Fire Weather Watch for wind and low relative humidity, which is in effect from Sunday morning through Sunday afternoon. * AFFECTED AREA...Fire Weather Zones 250 and 251. * TIMING...For the first Fire Weather Watch, from Sunday morning through Sunday afternoon. For the second Fire Weather Watch, from Tuesday morning through Tuesday evening. * WINDS...Southwest winds to 10 to 20 mph with gusts to 30 Sunday. On Tuesday, winds increase with west winds 30 to 40 mph with gusts up to 60 mph. * RELATIVE HUMIDITY...10 to 15 percent Sunday. Possibly as low as 5 to 10 percent Tuesday. * 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 are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
Weather Topic: What are Altostratus Clouds?
Home - Education - Cloud Types - Altostratus Clouds
Next Topic: Cirrocumulus Clouds
Altostratus clouds form at mid to high-level altitudes
(between 2 and 7 km) and are created by a warm, stable air mass which causes
water vapor
to condense as it rise through the atmosphere. Usually altostratus clouds are
featureless sheets characterized by a uniform color.
In some cases, wind punching through the cloud formation may give it a waved
appearance, called altostratus undulatus. Altostratus clouds
are commonly seen with other cloud formations accompanying them.
Next Topic: Cirrocumulus Clouds
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