Weather Alert in Texas
Blowing Dust Advisory issued February 17 at 2:01PM CST until February 17 at 7:00PM CST by NWS Lubbock TX
AREAS AFFECTED: Parmer; Castro; Swisher; Briscoe; Bailey; Lamb; Hale; Cochran; Hockley; Lubbock
DESCRIPTION: * WHAT...For the High Wind Warning, southwest winds 35 to 45 mph with some gusts to 65 mph expected. For the Blowing Dust Advisory, visibility between one-quarter and one mile in blowing dust. * WHERE...Bailey, Cochran, Hale, Hockley, Lamb, Lubbock, Briscoe, Castro, Parmer, and Swisher Counties. * WHEN...Until 7 PM CST this evening. * IMPACTS...Hazardous driving conditions due to reduced visibility. High winds may move loose debris, damage property and cause power outages. Travel could be difficult, especially for high profile vehicles.
INSTRUCTION: Persons with respiratory problems should make preparations to stay indoors until the storm passes. Be ready for a sudden drop in visibility to near zero. If you encounter blowing dust or blowing sand on the roadway or see it approaching, pull off the road as far as possible and put your vehicle in park. Turn the lights all the way off and keep foot off the brake pedal. Remember, 'Pull Aside, Stay Alive'. People are urged to secure loose objects that could be blown around or damaged by the wind.
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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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