Weather Alert in Illinois
Flood Advisory issued July 1 at 2:01AM CDT until July 1 at 4:00AM CDT by NWS Paducah KY
AREAS AFFECTED: Edwards, IL; Wabash, IL
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall will gradually recede. * WHERE...Portions of southeast and southern Illinois, including the following counties, Edwards and Wabash. * WHEN...Until 400 AM CDT. * IMPACTS...Minor flooding in low-lying and poor drainage areas. * ADDITIONAL DETAILS... - At 154 AM CDT, Doppler radar showed heavy rain due to thunderstorms had moved out of the area. Overflowing poor drainage areas causing minor flooding in the advisory area will slowly improve through 4am. Between 1.5 and 3 inches of rain have fallen. - Flooding impacts will continue but gradually improve with no additional rainfall expected. - Some locations that will experience flooding include... Mount Carmel, Albion, Grayville, Lancaster, West Salem, Allendale, Bellmont, Bone Gap, Keensburg and Browns. - http://www.weather.gov/safety/flood
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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