Weather Alert in Texas
Severe Thunderstorm Warning issued May 6 at 2:34AM CDT until May 6 at 3:30AM CDT by NWS San Angelo TX
AREAS AFFECTED: Schleicher, TX; Tom Green, TX
DESCRIPTION: At 234 AM CDT, a severe thunderstorm was located 9 miles south of Christoval, moving northeast at 35 mph. HAZARD...Two inch hail and 60 mph wind gusts. SOURCE...Radar indicated. IMPACT...People and animals outdoors will be injured. Expect hail damage to roofs, siding, windows, and vehicles. Expect wind damage to roofs, siding, and trees. This severe storm will be near... Christoval around 240 AM CDT. Vancourt around 305 AM CDT. Other locations impacted by this severe thunderstorm include The Intersection Of Ranch Road 1828 And Ranch Road 915.
INSTRUCTION: A Tornado Watch remains in effect until 400 AM CDT for west central Texas. For your protection move to an interior room on the lowest floor of a building.
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Weather Topic: What are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
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