Weather Alert in Texas
Special Weather Statement issued April 24 at 10:04AM CDT by NWS San Angelo TX
AREAS AFFECTED: Callahan; Coleman
DESCRIPTION: At 1003 AM CDT, Doppler radar was tracking a cluster of strong thunderstorms along the Coleman-Callahan County Line near Oplin, moving northeast at 20 mph. HAZARD...Wind gusts up to 50 mph and nickel size hail. SOURCE...Radar indicated. IMPACT...Gusty winds could knock down tree limbs and blow around unsecured objects. Minor hail damage to vegetation is possible. This strong thunderstorm will be near... Rowden around 1015 AM CDT. Other locations impacted by this storm include Us- 283 Near The Coleman- Callahan County Line, Lake Coleman, Admiral, and I- 20 Near The Callahan-Eastland County Line. This includes Interstate 20 between Mile Markers 319 and 323.
INSTRUCTION: If outdoors, consider seeking shelter inside 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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