Weather Alert in Texas
Severe Thunderstorm Warning issued April 1 at 9:48PM CDT until April 1 at 10:30PM CDT by NWS San Angelo TX
AREAS AFFECTED: Haskell, TX; Jones, TX; Shackelford, TX; Throckmorton, TX
DESCRIPTION: SVRSJT The National Weather Service in San Angelo has issued a * Severe Thunderstorm Warning for... Southern Haskell County in west central Texas... Jones County in west central Texas... Northwestern Shackelford County in west central Texas... Southwestern Throckmorton County in west central Texas... * Until 1030 PM CDT. * At 947 PM CDT, severe thunderstorms were located along a line extending from near Tuxedo to near Truby, moving northeast at 45 mph. HAZARD...60 mph wind gusts and penny size hail. SOURCE...Radar indicated. IMPACT...Expect damage to roofs, siding, and trees. * Severe thunderstorms will be near... Stamford, Anson, Paint Creek, and Avoca around 950 PM CDT. Lueders, Lake Stamford Marina, and Nugent around 955 PM CDT. Other locations impacted by these severe thunderstorms include Funston, Big Country Baptist Assembly, Truby, and Tuxedo.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building. A Tornado Watch remains in effect until midnight CDT for west central Texas.
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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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