Weather Alert in Alabama
Flood Advisory issued February 26 at 8:15PM CST until February 26 at 11:15PM CST by NWS Birmingham AL
AREAS AFFECTED: Blount, AL; Etowah, AL; St. Clair, AL
DESCRIPTION: * WHAT...Urban and small stream flooding caused by excessive rainfall is expected over the next three hours. * WHERE...A portion of central Alabama, including the following counties, Blount, Etowah and St. Clair. * WHEN...Until 1115 PM CST. * IMPACTS...Minor flooding in low-lying and poor drainage areas. * ADDITIONAL DETAILS... - At 812 PM CST, Doppler radar indicated heavy rain due to thunderstorms moving over similar locations. This will cause urban and small stream flooding. - Some locations that will experience flooding include... Gadsden, Rainbow City, Oneonta, Attalla, Hokes Bluff, Blountsville, Cleveland, Glencoe, Sardis City, Locust Fork, Steele, Altoona, Snead, Susan Moore, Walnut Grove, Reece City, Allgood, Fairview, Hayden and Nectar.
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Be especially cautious at night when it is harder to recognize the dangers of flooding.
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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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