Weather Alert in Alabama
Flood Warning issued May 11 at 9:08PM CDT by NWS Mobile AL
AREAS AFFECTED: Clarke, AL; Washington, AL
DESCRIPTION: ...The Flood Warning is extended for the following river in Alabama... Tombigbee River Near Leroy affecting Washington and Clarke Counties. For the Tombigbee River...including Coffeeville Dam - upstream, Coffeeville Dam, Leroy...Minor flooding is forecast. * WHAT...Minor flooding is forecast. * WHERE...Tombigbee River near Leroy. * WHEN...From Tuesday morning until further notice. * IMPACTS...At 24 feet, flooding of low lying farm and pasturelands begins. Cattle in low lying areas should be moved to higher ground. Water approaches low lying roads on west side of river. * ADDITIONAL DETAILS... - At 8:00 PM CDT Sunday the stage was 20.0 feet. - Forecast...The river is expected to rise above flood stage Tuesday morning and continue rising to 25.7 feet Thursday evening. Additional rises are possible thereafter. - Flood stage is 24 feet.
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Additional information is available at www.weather.gov/mob. Click on the Rivers and Lakes menu for forecasts and observations.
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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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