Weather Alert in Texas
Severe Thunderstorm Warning issued April 1 at 7:02PM CDT until April 1 at 8:00PM CDT by NWS San Angelo TX
AREAS AFFECTED: Fisher, TX; Jones, TX; Nolan, TX
DESCRIPTION: SVRSJT The National Weather Service in San Angelo has issued a * Severe Thunderstorm Warning for... Northwestern Jones County in west central Texas... Northwestern Nolan County in west central Texas... Fisher County in west central Texas... * Until 800 PM CDT. * At 702 PM CDT, a severe thunderstorm was located over Dunn, or 9 miles southeast of Snyder, moving northeast at 50 mph. HAZARD...70 mph wind gusts and quarter size hail. SOURCE...Radar indicated. IMPACT...Hail damage to vehicles is expected. Expect considerable tree damage. Wind damage is also likely to mobile homes, roofs, and outbuildings. * This severe thunderstorm will be near... Hobbs around 715 PM CDT. Rotan around 725 PM CDT. Roby around 730 PM CDT. Hamlin around 750 PM CDT. Other locations impacted by this severe thunderstorm include The Intersection Of Us-180 And Ranch Road 126, Us-84 Near The Nolan- Fisher County Line, I-20 Near The Nolan- Mitchell County Line, Hitson, Gannon, Lake Sweetwater, Camp Boothe Oaks, Busby, and Capitola. This includes Interstate 20 between Mile Markers 229 and 254.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building.
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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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