Weather Alert in Kansas
Fire Weather Watch issued February 14 at 12:07PM MST until February 17 at 8:00PM MST by NWS Goodland KS
AREAS AFFECTED: Rawlins; Sherman
DESCRIPTION: For Sunday, southwest winds of 15-25 mph are forecast to begin 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 Zones 002 Rawlins and 013 Sherman. * 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...For Sunday, southwesterly winds of 15 to 25 mph. For Tuesday, southwest 25 to 35 mph with gusts up to 55 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 weathesouthwest 30 to 40 mph with gusts up to 65 mph.Sr 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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