Weather Alert in Ohio
Flood Warning issued May 8 at 9:14PM EDT until May 9 at 11:00AM EDT by NWS Cleveland OH
AREAS AFFECTED: Holmes, OH; Wayne, OH
DESCRIPTION: ...The Flood Warning continues for the following rivers in Ohio... Killbuck Creek Near Killbuck affecting Holmes and Wayne Counties. For the Killbuck Creek...including Killbuck...Minor flooding is forecast. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Killbuck Creek near Killbuck. * WHEN...Until late tomorrow morning. * IMPACTS...At 15.0 feet, Several low lying roads in Holmes County including Township Roads 91 and 92, and County Roads 621 and 622 are flooded. * ADDITIONAL DETAILS... - At 9:00 PM EDT Thursday the stage was 15.3 feet. - Forecast...The river is expected to fall below flood stage late tonight and continue falling to 11.3 feet Tuesday morning. - Flood stage is 15.0 feet. - Please visit www.weather.gov/safety/flood for flood safety and preparedness information.
INSTRUCTION: Motorists should not attempt to drive around barricades or drive cars through flooded areas. Additional information is available at www.weather.gov/cle. The next statement will be issued Friday morning at 715 AM EDT.
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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
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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