Weather Alert in Texas
Severe Thunderstorm Warning issued August 2 at 3:38PM CDT until August 2 at 4:45PM CDT by NWS Fort Worth TX
AREAS AFFECTED: Bell, TX; Milam, TX
DESCRIPTION: SVRFWD The National Weather Service in Fort Worth has issued a * Severe Thunderstorm Warning for... Central Milam County in central Texas... Southeastern Bell County in central Texas... * Until 445 PM CDT. * At 337 PM CDT, severe thunderstorms were located along a line extending from near Buckholts to near Rockdale to near Tanglewood, moving east at 10 mph. A second thunderstorm capable of producing severe winds was located 1 mile east of Little River-Academy, moving southeast at 20 mph. HAZARD...60 mph wind gusts and nickel size hail. SOURCE...Radar indicated. IMPACT...Expect damage to roofs, siding, and trees. * Severe thunderstorms will be near... Rockdale, Buckholts, and Alcoa Lake around 345 PM CDT. Other locations impacted by these severe thunderstorms include Minerva, Ben Arnold, Cyclone, Sharp, Hoyte, Yarrelton, Pettibone, Milano, Silver City, and Edgeworth.
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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