Weather Alert in Oklahoma
Severe Thunderstorm Warning issued August 29 at 7:13PM CDT until August 29 at 8:30PM CDT by NWS Amarillo TX
AREAS AFFECTED: Cimarron, OK; Texas, OK
DESCRIPTION: SVRAMA The National Weather Service in Amarillo has issued a * Severe Thunderstorm Warning for... Western Texas County in the Panhandle of Oklahoma... Eastern Cimarron County in the Panhandle of Oklahoma... * Until 830 PM CDT. * At 712 PM CDT, a severe thunderstorm was located 4 miles west of Eva, or 15 miles south of Elkhart, moving southeast at 20 mph. HAZARD...60 mph wind gusts and half dollar size hail. SOURCE...Radar indicated. IMPACT...Minor damage to roofs, siding, and trees is possible. Hail damage to vehicles is expected. * Locations impacted include... Guymon, Keyes, Eva, Griggs, and Sturgis.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building. Large hail, damaging wind, and continuous cloud to ground lightning are occurring with this storm. Move indoors immediately. Lightning is one of nature's leading killers. Remember, if you can hear thunder, you are close enough to be struck by lightning. Torrential rainfall is occurring with this storm, and may lead to flash flooding. Do not drive your vehicle through flooded roadways.
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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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