Weather Alert in Texas
Severe Thunderstorm Warning issued September 5 at 10:50PM CDT until September 5 at 11:30PM CDT by NWS Fort Worth TX
AREAS AFFECTED: Dallas, TX
DESCRIPTION: SVRFWD The National Weather Service in Fort Worth has issued a * Severe Thunderstorm Warning for... Dallas County in north central Texas... * Until 1130 PM CDT. * At 1049 PM CDT, severe thunderstorms were located along a line extending from Coppell to Dallas Love Field to near Duncanville, moving east at 25 mph. HAZARD...60 mph wind gusts and nickel size hail. SOURCE...Radar indicated. IMPACT...Expect damage to roofs, siding, and trees. * Locations impacted include... Dallas, Garland, Irving, Grand Prairie, Mesquite, Carrollton, Richardson, Rowlett, Desoto, Grapevine, Cedar Hill, Wylie, Coppell, Duncanville, Lancaster, Farmers Branch, Balch Springs, University Park, Sachse, and Seagoville. This includes the following highways... Interstate 35E between mile markers 416 and 445. Interstate 20 between mile markers 454 and 485. Interstate 30 between mile markers 32 and 64. Interstate 45 between mile markers 274 and 284.
INSTRUCTION: For your protection get inside a sturdy structure and stay away from windows.
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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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