Weather Alert in Nebraska
Flood Advisory issued September 1 at 11:56AM CDT until September 1 at 3:00PM CDT by NWS Omaha/Valley NE
AREAS AFFECTED: Jefferson, NE; Saline, NE
DESCRIPTION: * WHAT...Small stream flooding caused by excessive rainfall is expected. * WHERE...A portion of southeast Nebraska, including the following counties, Jefferson and Saline. * WHEN...Until 300 PM CDT. * IMPACTS...Minor flooding in low-lying and poor drainage areas. Rises in small streams and normally dry arroyos. Water over roadways. * ADDITIONAL DETAILS... - At 1153 AM CDT, Doppler radar indicated heavy rain due to thunderstorms this morning, bringing small stream flooding. Between 2 and 4 inches of rain have fallen. - Some locations that will experience flooding include... Fairbury, Wilber, Plymouth, Western, Daykin, Endicott, Jansen, Tobias, Swanton, Harbine, Cub Creek Recreational Area, Swan Creek Wildlife Management Area, The Highway 41 and 15 South Junction, Crystal Springs Campground, Willard Meyer Recreation Area, Rock Creek Station State Historical Park, Camp Jefferson, Gladstone and Swan Creek Reservoir Number 2.
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Be aware of your surroundings and do not drive on flooded roads.
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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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