Weather Alert in Illinois
Flood Warning issued March 14 at 12:02PM CDT until March 18 at 4:00PM CDT by NWS Paducah KY
AREAS AFFECTED: Gallatin, IL; Wayne, IL; White, IL
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Illinois... Little Wabash River at Carmi affecting Gallatin, Wayne and White Counties. .Recent heavy rainfall is causing the Little Wabash River to rise, with an expected crest at Carmi just 28.1 feet tomorrow morning. It will then fall below flood stage Tuesday evening. For the Little Wabash River...including Carmi...Minor flooding is forecast. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Little Wabash River at Carmi. * WHEN...Until Wednesday afternoon. * IMPACTS...At 27.0 feet, The inundation of county roads begins. * ADDITIONAL DETAILS... - At 11:30 AM CDT Saturday the stage was 28.0 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 11:30 AM CDT Saturday was 28.0 feet. - Forecast...The river is expected to rise to a crest of 28.1 feet tomorrow morning. It will then fall below flood stage late Wednesday morning. - Flood stage is 27.0 feet.
INSTRUCTION: Motorists should not attempt to drive around barricades or drive cars through flooded areas. Additional information is available at www.weather.gov.
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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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