Weather Alert in Texas
Special Weather Statement issued May 25 at 10:31PM CDT by NWS Amarillo TX
AREAS AFFECTED: Hutchinson; Roberts; Carson; Gray; Wheeler; Donley; Collingsworth
DESCRIPTION: At 1031 PM CDT, Doppler radar was tracking strong thunderstorms along a line extending from 4 miles east of Stinnett to 3 miles northwest of Pampa to 4 miles northeast of Lake Mcclellan to 5 miles south of Clarendon. Movement was east at 35 mph. HAZARD...Wind gusts up to 50 mph. SOURCE...Radar indicated. IMPACT...Gusty winds could knock down tree limbs and blow around unsecured objects. Locations impacted include... Howardwick, Hedley, Lelia Lake, Lake Mcclellan, Lefors, Kellerville, Miami, Clarendon, Skellytown, Mclean, Pampa, Kingsmill, Alanreed, Codman, Borger, and Greenbelt Lake. This includes Interstate 40 between mile markers 120 and 155.
INSTRUCTION: If outdoors, consider seeking shelter inside a building. Torrential rainfall is also occurring with these storms and may lead to localized flooding. Do not drive your vehicle through flooded roadways. A Severe Thunderstorm Watch remains in effect until 100 AM CDT for the Panhandle of 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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