Weather Alert in Indiana
Flood Warning issued March 6 at 11:35AM CST until March 15 at 3:25AM CDT by NWS Paducah KY
AREAS AFFECTED: Posey, IN; Union, KY
DESCRIPTION: ...The National Weather Service in Paducah KY has issued a Flood Warning for the following river in Indiana...Kentucky... Ohio River at J.T. Myers Dam and Mount Vernon. .Recent and expected heavy rains are projected to raise water levels into flood next week on the Ohio River at Mount Vernon and J.T. Myers Dam. Both locations are projected to crest in minor flood later in the week. For the Ohio River...including Mount Vernon, J.T. Myers Dam...Minor flooding is forecast. * WHAT...Minor flooding is forecast. * WHERE...Ohio River at J.T. Myers Dam. * WHEN...From Monday morning to Sunday, March 15. * ADDITIONAL DETAILS... - At 11:00 AM CST Friday the stage was 27.1 feet. - Forecast...The river is expected to rise above flood stage Monday morning to a crest of 38.9 feet early Thursday afternoon. It will then fall below flood stage Saturday, March 14. - Flood stage is 37.0 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.
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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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