Weather Alert in Texas
Severe Thunderstorm Warning issued September 5 at 6:49PM CDT until September 5 at 7:45PM CDT by NWS Fort Worth TX
AREAS AFFECTED: Collin, TX; Denton, TX
DESCRIPTION: SVRFWD The National Weather Service in Fort Worth has issued a * Severe Thunderstorm Warning for... Eastern Denton County in north central Texas... Western Collin County in north central Texas... * Until 745 PM CDT. * At 649 PM CDT, a severe thunderstorm was located over Cross Roads, or near Corinth, moving east at 20 mph. HAZARD...65 mph wind gusts and nickel size hail. SOURCE...Radar indicated. IMPACT...Expect damage to roofs, siding, and trees. * This severe thunderstorm will be near... Frisco, Little Elm, Prosper, Celina, and Cross Roads around 655 PM CDT. McKinney around 715 PM CDT. Other locations impacted by this severe thunderstorm include Weston, Lewisville Lake, Oak Point, Lincoln Park, Lakewood Village, Grapevine Lake, and Providence Village. This includes the following highways... Interstate 35 between mile markers 468 and 476. Interstate 35W between mile markers 81 and 85. Interstate 35E between mile markers 446 and 466.
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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